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  <front>
    <journal-meta><journal-id journal-id-type="publisher">NHESS</journal-id><journal-title-group>
    <journal-title>Natural Hazards and Earth System Sciences</journal-title>
    <abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1684-9981</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/nhess-23-871-2023</article-id><title-group><article-title>Sensitivity analysis of a built environment exposed to the<?xmltex \hack{\break}?> synthetic monophasic viscous debris flow impacts with<?xmltex \hack{\break}?> 3-D numerical simulations</article-title><alt-title>Sensitivity analysis of a built environment exposed to the debris flow impacts</alt-title>
      </title-group><?xmltex \runningtitle{Sensitivity analysis of a built environment exposed to the debris flow impacts}?><?xmltex \runningauthor{X. Huang et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1 aff2">
          <name><surname>Huang</surname><given-names>Xun</given-names></name>
          <email>huangxun@cqnu.edu.cn</email>
        <ext-link>https://orcid.org/0000-0003-3806-140X</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Zhang</surname><given-names>Zhijian</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3 aff4">
          <name><surname>Xiang</surname><given-names>Guoping</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>Geography and Tourism College, Chongqing Normal University, Chongqing 401331, China</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Chongqing Key Laboratory of Surface Process and Environment Remote
Sensing in the Three Gorges Reservoir Area, Chongqing Normal University,
Chongqing 401331, China</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>405 Geological Brigade of Sichuan Bureau of Geology &amp; Mineral
Resources, Dujiangyan 611830, China</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>State Key Laboratory of Geohazard Prevention and Geoenvironment
Protection,<?xmltex \hack{\break}?> Chengdu University of Technology, Chengdu 610059, China</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Xun Huang (huangxun@cqnu.edu.cn)</corresp></author-notes><pub-date><day>1</day><month>March</month><year>2023</year></pub-date>
      
      <volume>23</volume>
      <issue>2</issue>
      <fpage>871</fpage><lpage>889</lpage>
      <history>
        <date date-type="received"><day>16</day><month>June</month><year>2022</year></date>
           <date date-type="rev-request"><day>20</day><month>July</month><year>2022</year></date>
           <date date-type="rev-recd"><day>25</day><month>December</month><year>2022</year></date>
           <date date-type="accepted"><day>14</day><month>February</month><year>2023</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2023 Xun Huang et al.</copyright-statement>
        <copyright-year>2023</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023.html">This article is available from https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023.html</self-uri><self-uri xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d1e125">The characteristics of exposed built environments have a
significant effect on debris flow impacts on buildings, but knowledge about
their interactions is still limited. This paper presents a sensitivity
analysis on the peak impact forces on a whole building resulting from the
built environment parameters, including the orientation, opening scale of
the target building, and azimuthal angle and distance of surrounding
buildings. The impact forces were obtained from the monophasic viscous
debris flow with a synthetic and simplified hydrograph using the FLOW-3D
model, a computational fluid dynamics approach, verified through the
physical modeling results. The results show that the surrounding buildings'
properties have significant roles in determining the peak impact forces. A
shielding effect or canalization effect, which reduces or increases impact
forces, respectively, can be produced by changing the azimuth angle. A
deflection wall for building protection is recommended according to the
shielding effect. A narrowed flow path, determined by both the azimuth angle and distance, has a significant effect on the variation in impact forces. In
addition, it is concluded that a splitting wedge should be designed
following a criterion of avoiding the highest flow depth – the maximum
approaching angle – appearing near the longest wall element. The protruding parts caused by changing the building's orientation contribute to increasing
impact loads within a shielding area. A limited opening scale effect is
observed on the whole building if there is sufficient time for material
intrusion. The insights gained contribute to a better understanding of
building vulnerability indicators and local migration design against debris
flow hazard.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <p id="d1e137">In mountain environments, buildings are the elements of greatest concern
with regard to debris flow hazard risks (Zeng et al., 2015; Fuchs et al.,
2019; Luo et al., 2020). Compared to strong structures such as railway
bridges, common residential buildings are more easily damaged by debris
flows (Hu et al., 2012; Huang and Tang, 2014). Furthermore, the damage to
buildings has been demonstrated to contribute greatly to casualties and
property loss based on a large number of catastrophic debris flow events
(Tang et al., 2011; Zhang et al., 2018; Chen et al., 2021). In recent
decades, the understanding, assessment, and eventual reduction in building
exposure and vulnerability have been brought into focus in mountain hazard
mitigation (Holub and Fuchs, 2009; Fuchs et al., 2015, 2017).</p>
      <p id="d1e140">In the classical S-shaped vulnerability curves, a quantitative assessment
approach based on interactions between process intensities and building
damage, considerable ranges in the loss ratio were found for moderate
process intensities (Fuchs et al., 2012). This is in good agreement with<?pagebreak page872?> the
fact that two buildings located exactly at the same place, despite
experiencing the same process intensity, do not always suffer the same
degree of loss (Papathoma-Köhle, 2016; Papathoma-Köhle et al.,
2017). Process intensity is not decisive in terms of building damage, and
some building characteristics of the building itself and its surroundings
play critical roles in the degree of damage induced by debris flow. This
understanding has also been confirmed by the spatial distribution of
building damage ratios in the debris flow torrents of the Austrian Alps
(Fuchs et al., 2012).</p>
      <p id="d1e143">Currently, the characteristics of an exposed building, including the
orientation, openings and surrounding environments, have been reported to be
important to the impact forces of torrential hazards (Jakob et al., 2012;
Sturm et al., 2018a). As far as building orientation is concerned, it is
commonly recommended to individually analyze wall elements of different
orientations. It is widely accepted that walls with faces perpendicular to
the stream are generally exposed to higher dynamic pressures due to the
larger effective contact area (Mead et al., 2017; Manawasekara et al.,
2016). However, limited studies to date have examined the impact performance
of a whole building. In terms of building openings such as windows, doors
and light shafts, it is well established that the impact forces on the
building envelope tend to decrease once the flow penetrates openings
(Mazzorana et al., 2014; Gems et al., 2016). However, this process is
regarded to be at the expense of greater building loss due to the higher
impact forces on interior walls and greater indoor property losses
(Totschnig et al., 2011; Mead et al., 2017). Recent developments regarding
the surroundings of built environments have attracted much attention. The
existence of surrounding buildings definitely reduces the impact forces on a
particular building due to the deflection of the flow and the shielding of
the element at risk; however, this may also increase the impact forces by
redirecting or canalizing the flow and forcing the flow to impact the
building (Gao et al., 2017; Sturm et al., 2018b). Therefore, it remains
difficult to make a general statement regarding whether the effect of
surrounding buildings is negative or positive (Sturm et al., 2018a).</p>
      <p id="d1e146">Although considerable efforts have been devoted to the relationships between
building characteristics and debris flow impacts, only some simple trends,
rather than quantitative results about the effects of factors, have been
determined. Knowledge regarding the interactions between the built
environment parameters and impact loads is still limited, and considerable
research gaps still exist regarding (1) the identification of the built
environment parameters with the greatest influence on debris flow impacts,
(2) detailed explanations of each built environment factor and (3) the
interrelations between these parameters.</p>
      <p id="d1e150">Because field measurement of debris flow impacts is nearly impossible,
laboratory experiments and numerical modeling are regarded as feasible
alternatives for capturing interactions, and they may provide insights into
the impact of debris flows in the interior and against the exterior of
buildings (Gems et al., 2016; Papathoma-Köhle, 2016). In this study, a
sensitivity analysis was conducted based on 3-D numerical simulation, and
the effects of various built environment factors on the impact forces of
debris flows were quantitatively analyzed and compared. Debris flow
numerical simulations were conducted using the FLOW-3D model, a commercial
computational fluid dynamics (CFD) program. Kim et al. (2021) conducted a
sensitivity analysis of five parameters for fine sediment trapping and
energy reduction with a debris flow slit-type barrier via a FLOW-3D
numerical model and metamodels. These kinds of methods offer opportunities
for performing a sensitivity analysis with limited data (Kim et al., 2019, 2021). These results can be applied to determine the indicators
and to improve weightings for reliable building vulnerability assessment and
to enhance the knowledge about built environment improvement and local
migration design.</p>
      <p id="d1e153">In the following, the reliability of the numerical model was first confirmed
by comparison with a physical dam-break experiment. A sensitivity analysis
was then performed using metamodels and global sensitivity analysis (GSA).
The built environment parameters considered in this study were the
orientation (Or) and opening scale (Op)
of the target building and the azimuthal angle (<inline-formula><mml:math id="M1" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) and
distance (<inline-formula><mml:math id="M2" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) of the surrounding buildings. Finally, the
effects of each parameter and their interactions on the peak impact forces
of the overall building were explained in detail.</p>
</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Numerical modeling of debris flow</title>
<sec id="Ch1.S2.SS1">
  <label>2.1</label><title>Model description</title>
      <p id="d1e185">The identification of complex geometry and 3-D flow tracking
are the key steps in the process-response simulation between buildings and
debris flows. However, the current numerical codes used for debris flow
simulations consider the flow depth to be small relative to the tangential
length scale and simplify this factor to represent shallow water flow. They
have only second-order accuracy in space, as the effects of complex
3-D topography and the vertical mobility of debris flows are
not considered (Y. Zhang et al., 2021). To avoid the abovementioned
limitations, it is necessary to use an efficient 3-D numerical approach to
accurately capture the debris flow behaviors considering the influences of
building geometry.</p>
      <p id="d1e188">FLOW-3D, a 3-D finite-volume-based CFD model, is considered
one of the most efficient tools for predicting hydraulic phenomena with
strong turbulent components and inconsistent free water surfaces. FLOW-3D
was designed to address the Reynolds-averaged Navier–Stokes equations (RANS)
(Jones and Launder, 1972), implementing the volume of fluid (VOF) methods
(Hirt and Nichols, 1981) and fractional area–volume obstacle representation
(FAVOR) (Hirt and Sicilian, 1985). The advanced TruVOF method can be used
to precisely track the 3-D transient free fluid<?pagebreak page873?> surface. Its unique FAVOR mesh processing technology can define independent and complex
geometry within the structured mesh and avoid the shortcomings of the
traditional finite difference method in complex boundary fitting (Y. Zhang et
al., 2021). The FAVOR processor can generate area fractions for each cell
face in the grid by determining which corners of the face are inside of a
defined geometry and incorporate geometry effects into the governing
equations. As a result of a robust capacity to deal with the data in both
the fluid and solid phases, the FLOW-3D code is considered to be appropriate
for analyzing the interactions between debris flows and exposed buildings.</p>
      <p id="d1e191">In this study, the renormalized group (RNG) model-based <inline-formula><mml:math id="M3" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M4" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula>
turbulence model and the general moving objects (GMO) model are applied to
build a fluid–solid-coupled model of the debris flow impact. The RNG
<inline-formula><mml:math id="M5" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M6" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula> model is a modification of the standard <inline-formula><mml:math id="M7" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M8" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula>
model, which takes the turbulent vortex into account and provides an
analytic formula for the Prandtl number, as well as an analytic formula for low
Reynolds number flow viscosity (Franco et al., 2021). These features make
the RNG model more reliable and accurate for a broader flow than the
standard <inline-formula><mml:math id="M9" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M10" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula> model (Yin et al., 2015). In recent years, the RNG
model has been applied in simulations of landslide surges (Yin et al., 2015;
Hu et al., 2020), the entrainment effects of debris avalanches (Hu et al.,
2019), dam-break floods (Zhuang et al., 2020) and the runout characteristics
of debris flows (Y. Zhang et al., 2021), with good results.</p>
      <p id="d1e251">The turbulent kinetic energy and the turbulence dissipation balance
equations of the RNG <inline-formula><mml:math id="M11" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M12" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula> model in FLOW-3D are as following:

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mathvariant="normal">T</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:mo>∂</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:mfrac></mml:mstyle></mml:mrow></mml:mfenced><mml:mo>=</mml:mo></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mspace width="1em" linebreak="nobreak"/><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi mathvariant="normal">CDIS</mml:mi><mml:mn mathvariant="normal">1</mml:mn><mml:mo>⋅</mml:mo><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:mi mathvariant="normal">CDIS</mml:mi><mml:mn mathvariant="normal">3</mml:mn><mml:mo>⋅</mml:mo><mml:msub><mml:mi>G</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">Diff</mml:mi><mml:mi mathvariant="italic">ε</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:mi mathvariant="normal">CDIS</mml:mi><mml:mn mathvariant="normal">2</mml:mn><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msubsup><mml:mi mathvariant="italic">ε</mml:mi><mml:mi mathvariant="normal">T</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mrow></mml:mtd></mml:mlabeledtr></mml:mtable></mml:math></disp-formula>

            where <inline-formula><mml:math id="M14" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the turbulent kinetic energy; <inline-formula><mml:math id="M15" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi mathvariant="normal">F</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the fractional volume open to flow; and <inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:msub><mml:mi>A</mml:mi><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M17" display="inline"><mml:mrow><mml:msub><mml:mi>A</mml:mi><mml:mi>y</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M18" display="inline"><mml:mrow><mml:msub><mml:mi>A</mml:mi><mml:mi>z</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are the fractional area open to flow in the <inline-formula><mml:math id="M19" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M20" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math id="M21" display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> directions, respectively. <inline-formula><mml:math id="M22" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the turbulent kinetic energy production term, <inline-formula><mml:math id="M23" display="inline"><mml:mrow><mml:msub><mml:mi>G</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the buoyancy production term, Diff is the diffusion term, and <inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the turbulence dissipation term. In the RNG model of FLOW-3D, CDIS1 and CDIS3 are dimensionless user-adjustable parameters that have defaults of 1.42 and 0.2, respectively,
and CDIS2 is determined from <inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M26" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (Flow Science, Inc., 2014).</p>
      <p id="d1e750">In this study, a series of debris flow simulations based on the RNG model
with various building characteristics were executed. From the
characteristics of the RNG <inline-formula><mml:math id="M27" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M28" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula> model, the type of debris flow
involved in this study was determined as mudflow or viscous debris flow, in
which a single-phase fluid was assumed and solid particles were treated as
suspension and mixed with the fluid phase well. The division between solid
and fluid was assumed to be difficult; therefore, the granular deposition
was not considered in this study.</p>
      <p id="d1e767">With the help of the GMO model in FLOW-3D, the combined hydraulic force due to
normal pressure and shear stress can be calculated in the space system. The
normal pressure and shear force of an impacted object in <inline-formula><mml:math id="M29" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M30" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math id="M31" display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula>
directions can be gained at each time step. Due to the complex geometry and
variable built environments, the impacted elements of target building were
changing in the different scenarios. In this study, therefore, the target
building was treated as a whole bearing structure to keep consistency of
analysis. All over the grids covering building surface would be calculated
when contacting with the flow. The GMO model can simulate the rigid body
motion, which is either user prescribed or dynamically coupled with fluid
flow. In this study, the target building and surrounding buildings were all
prescribed to be the fixed and nondeformable rigid models. The raw impact
force data were collected at an interval of 0.001 s from the numerical code and averaged manually over 10 points (0.01 s) to reduce uncertainty (Song et al., 2021).</p>
</sec>
<sec id="Ch1.S2.SS2">
  <label>2.2</label><title>Model validation</title>
      <p id="d1e799">The interaction between a dam break and the structure has become a classic
benchmark for the validation of fluid–structure interaction (Liu et al.,
2021). The accuracy of the model will be validated by means of the
experimental setup previously used in Gomez-Gesteira and Dalrymple (2004).
This experiment has been referred to as a “bore in a box”, where it was a
dam-break and structure-impact problem confined within a rectangular box.
The geometric dimensions of the experimental model are shown in Fig. 1. The
rectangular tank is 1.60 m long, 0.61 m wide and 0.75 m high. The tank is
considered to be a smooth surface, and its surface roughness (<inline-formula><mml:math id="M32" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>) is set to 0 m
(Liu et al., 2021). The volume of water initially contained behind a thin
gate at one end of the box is 0.4 m long, 0.61 m wide and 0.3 m high. An
initial layer of water (approximately 1 cm deep) existed on the bottom of
the tank. The obstacle, which is 0.12 m <inline-formula><mml:math id="M33" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 0.12 m <inline-formula><mml:math id="M34" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 0.75 m
in size, is placed 0.5 m downstream of the gate and 0.24 m from the nearest
sidewall of the tank. The surface roughness of the obstacle is not
determined. Therefore, <inline-formula><mml:math id="M35" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">o</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (0, 0.001, 0.002 or 0.003 m) is selected for sensitivity analysis to determine if this parameter could reasonably reflect
the macromechanical behaviors of the dam-break test. The time history of
the impact force on the structure was measured with a load cell.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><?xmltex \currentcnt{1}?><?xmltex \def\figurename{Figure}?><label>Figure 1</label><caption><p id="d1e836">The geometric dimensions of the experimental dam-break model.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f01.jpg"/>

        </fig>

      <?pagebreak page874?><p id="d1e845">In the numerical simulation, the analysis domain was discretized into a grid
with a cell size of 0.01 m, which was equal to a cube with a 0.01 m side in a 3-D
model. The fluid properties were set to be the density of 1000 kg m<inline-formula><mml:math id="M36" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>
and viscosity of 0.001 Pa s. The motion of fluid was computed by
means of the RNG <inline-formula><mml:math id="M37" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>-<inline-formula><mml:math id="M38" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula> model in FLOW-3D. The obstacle and gate were
controlled by the GMO module; specifically this obstacle was set as a fixed
and nondeformable rigid body, and the gate was prescribed to be lifted 0.3 m along the <inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:msup><mml:mi>z</mml:mi><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> direction. The time history of impact forces and the
corresponding dynamic processes were selected to validate the accuracy of
the numerical simulation. The direction of the force was considered positive
when exerted in the <inline-formula><mml:math id="M40" display="inline"><mml:mrow><mml:msup><mml:mi>y</mml:mi><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> direction.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2" specific-use="star"><?xmltex \currentcnt{2}?><?xmltex \def\figurename{Figure}?><label>Figure 2</label><caption><p id="d1e899">The dam-break simulation <bold>(a)</bold> comparison between numerical (dotted lines) and experimental values (red line) of the force exerted on the
structure. <bold>(b)</bold> Wave evolution: (<inline-formula><mml:math id="M41" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M42" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 0.32 s) the wave is colliding with the front of the obstacle; (<inline-formula><mml:math id="M43" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M44" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 0.58 s) the wave is wrapping around the structure, colliding together and continues moving toward the tank wall; and (<inline-formula><mml:math id="M45" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M46" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.44 s) the reflected wave is hitting the back of the obstacle.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f02.jpg"/>

        </fig>

      <p id="d1e957">Figure 2a shows the general agreement of numerical forces obtained by means of the RNG and GMO coupled model with experimental data, particularly the
positions of both peaks, which correspond to the wave hitting the front and
the back of the structure and were reasonably reproduced by the numerical
model. This indicates that the impact force has a very low sensitivity to
<inline-formula><mml:math id="M47" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mi mathvariant="normal">o</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>; this study does not pay too much attention to the value of this parameter, and the surface roughness (<inline-formula><mml:math id="M48" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>) of all the impacted objects in
the numerical simulation is set to 0 m. Figure 2b shows the evolution of the wave
generated by the dam break and the initial layer of water on the bottom. At
<inline-formula><mml:math id="M49" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M50" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 0.32 s, the wave is colliding with the front of the obstacle. At <inline-formula><mml:math id="M51" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M52" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 0.58 s, the wave is wrapping around the structure, colliding together and continues moving toward the tank wall. At <inline-formula><mml:math id="M53" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M54" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.44 s, the reflected wave
is hitting the back of the obstacle.</p>
</sec>
<sec id="Ch1.S2.SS3">
  <label>2.3</label><title>Numerical model setup</title>
      <p id="d1e1029">As shown in Fig. 3, a depositional fan model with a length of 120 m, width
of 120 m and monogradient of 5<inline-formula><mml:math id="M55" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> was numerically constructed. This
deposition fan was treated as a rigid bed model; therefore, the bed material
scour would not happen in this study. To sum up, the bed variation induced
by sediment transport processes, including sediment deposition and bed
scour, was not considered. The surface roughness (<inline-formula><mml:math id="M56" display="inline"><mml:mi>k</mml:mi></mml:math></inline-formula>) of 0.05 m was set,
meaning that the deposition fan surface was roughened with 5 cm diameter
particles, for the representation of the natural environment surrounding
mountainous buildings.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><?xmltex \currentcnt{3}?><?xmltex \def\figurename{Figure}?><label>Figure 3</label><caption><p id="d1e1050">Overview of the components of a 3-D deposition fan
model for debris flow impact simulation on buildings.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f03.png"/>

        </fig>

      <p id="d1e1059">The realistic debris flow inflow discharge and duration are essential for a
truthful analysis of impact forces. A 3-D numerical simulation with a
realistic hydrograph, however, needs a large amount of computer memory and
processing time. It is difficult to accept in the sensitivity analysis,
in which the sufficient experimental groups are required. In this study, a
synthetic and simplified inflow hydrograph was set at the top center of the
deposition fan. Specifically, the debris flow discharge was fixed as 500 m<inline-formula><mml:math id="M57" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> s<inline-formula><mml:math id="M58" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, which can be of some interest for a large magnitude of
debris flow, and the inflow duration was limited to 5 s. The inflow cross
section was rectangular, with a channel base width of 20 m, flow depth of
2.5 m, inclination angle of 5<inline-formula><mml:math id="M59" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and an initial velocity of 10 m s<inline-formula><mml:math id="M60" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>. In consideration of the distance between the inflow cross section and
target building, a computation time of 15 s, triple the inflow duration,
was set for the FLOW-3D modeling, to ensure all the debris flow can flow
through the target building. The peak impact force was treated as the
maximum value in a relatively complete impact process. In order to compare
with some realistic building damage cases, for example the Qipan gully and
Zhouqu debris flows in the west of China, the rheological properties of
the numerical model was set as the viscous debris flow. Therefore, the debris
flow density was set as 2000 kg m<inline-formula><mml:math id="M61" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and viscosity was empirically 1.0 Pa s (Takahashi, 2007).</p>
      <p id="d1e1117">The target and surrounding building models, with a length of 15 m, width of
10 m, height of 6 m (equal to two floors) and wall thickness of 0.35 m, were
designed in accordance with representative buildings in the mountainous
areas of  western China. To maintain a balance between the computational
accuracy and time cost, the whole computation domain was discretized at
intervals of 0.5 m. The planar center of the target building was set at 80 m
downstream of the debris flow inflow, as shown in Fig. 3. The embedded
domain of the target building should be refined further following two
principles: (1) its cell size must be less than the wall thickness of 0.35 m. This is because it is possible that the wall geometry may intersect a cell face more than once in the case of the building rotating, and the corresponding cell edge is assumed to be either fully inside the object or fully outside; some lacks of wall surface will be produced. (2) The boundaries of the
embedded and external meshes must be overlapped for the computation
stability, that is, the external cell size is a multiple of embedded cell
size. To sum up, the cell size of the target building domain was determined as
0.25 m. The total number of computational cells was 1 645 600, and the
computer memory of a single simulation was about 20 GB.</p>
      <?pagebreak page875?><p id="d1e1120">Because the sensitivity analysis requires extensive simulation results to
consider the combinations of all the factors, the representative factors
that could be adjusted in the FLOW-3D simulation were chosen (Kim et al.,
2021). The orientation (Or) and opening scale (Op) of the target building and the azimuthal angle (<inline-formula><mml:math id="M62" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) and distance (<inline-formula><mml:math id="M63" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) of the surrounding
buildings with respect to the target building were considered to be the key
built environment parameters for debris flow impact loads.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><?xmltex \currentcnt{4}?><?xmltex \def\figurename{Figure}?><label>Figure 4</label><caption><p id="d1e1139">The schematic drawings of the target building and surrounding
buildings: <bold>(a)</bold> orientation of target building (Or), <bold>(b)</bold> opening scale of the target building (Op), and <bold>(c)</bold> azimuth angle (<inline-formula><mml:math id="M64" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) and distance (<inline-formula><mml:math id="M65" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) of surrounding
building with respect to the target building.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f04.png"/>

        </fig>

      <p id="d1e1171">In this study, the orientation (Or) of the target building
was defined as the angle between the building's long axis and the debris
flow's main flow path, as shown in red and green in Fig. 4a, and ranged from
0 to 90<inline-formula><mml:math id="M66" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. An orientation of 0<inline-formula><mml:math id="M67" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> meant that
the long axis of the building was parallel to the debris flow path, and the
perpendicular case was represented by an orientation of 90<inline-formula><mml:math id="M68" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. As
far as building openings are concerned, it is well known that several
features of openings are of great importance in terms of building damage,
such as which wall they are located on and their size, height and structure
(Gems et al., 2016; Faisal et al., 2018; Papathoma-Köhle et al., 2019).
However, it remains challenging to analyze these parameters with a single
model. In this study, the size of the opening was only selected to be
analyzed to reduce computing costs. As shown in Fig. 4b, two<?pagebreak page876?> symmetrical
openings with a constant height of 3 m were placed in wall A. Therefore, the
opening scale (Op) was defined as the proportion of the
total opening width (double <inline-formula><mml:math id="M69" display="inline"><mml:mi>w</mml:mi></mml:math></inline-formula>) to the length of wall A.</p>
      <p id="d1e1208">The azimuthal angle (<inline-formula><mml:math id="M70" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) of the surrounding buildings was
defined as the angle between the line of the geometric center of buildings
(e.g., line B–B' in Fig. 4c) and the main flow path (green line in Fig. 4c).
There were no surrounding buildings downstream of the target building.
Except for the scenario of an azimuthal angle of 0<inline-formula><mml:math id="M71" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, two surrounding
buildings were placed symmetrically on both sides of the target building.
The distance (<inline-formula><mml:math id="M72" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) between the surrounding building and
target building was defined as the straight-line distance between two points
located on the overlap between the line of the buildings' geometric centers
and building envelope, as shown by the orange line C–C' in Fig. 4c.</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <label>3</label><title>Sensitivity analysis</title>
<sec id="Ch1.S3.SS1">
  <label>3.1</label><title>Metamodel modeling</title>
      <p id="d1e1250">Abundant simulation results are required for assessing the effect of built
environment parameters on the debris flow impact force. Due to the
considerable time consumed and computational cost, a mathematical metamodel
was constructed using a small fraction of the simulation results. A
metamodel, referred to as a surrogate model, is a “model of a model”, a
simplified model of an actual model using mathematical construction.
Numerous accurate simulation results can be generated based on the metamodel
relation or algorithm between input and output (Booker et al., 1999; Hoffman
et al., 2003). Of the various metamodel modeling methods, the Kriging model
– or Gaussian process (GP) – is considered to be the most suitable for the
unbiased prediction of a deterministic model and is also fitted to
simulation I/O data obtained for global experimental areas (Kleijnen, 2016).
In this study, the GP was selected and executed through JMP<sup>®</sup>
Pro 16.0.0, a commercial statistical software designed by the SAS Institute Inc.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><?xmltex \currentcnt{1}?><label>Table 1</label><caption><p id="d1e1259">Simulation conditions.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="6">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="left" colsep="1"/>
     <oasis:colspec colnum="5" colname="col5" align="left"/>
     <oasis:colspec colnum="6" colname="col6" align="left"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Group</oasis:entry>
         <oasis:entry colname="col2">Number</oasis:entry>
         <oasis:entry rowsep="1" namest="col3" nameend="col4" align="center" colsep="1">Target building's properties </oasis:entry>
         <oasis:entry rowsep="1" namest="col5" nameend="col6" align="center">Surrounding buildings' properties </oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">of cases</oasis:entry>
         <oasis:entry colname="col3">Orientation</oasis:entry>
         <oasis:entry colname="col4">Opening scale</oasis:entry>
         <oasis:entry colname="col5">Azimuth angle</oasis:entry>
         <oasis:entry colname="col6">Distance</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2"/>
         <oasis:entry colname="col3">(Or, <inline-formula><mml:math id="M75" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col4">(Op)</oasis:entry>
         <oasis:entry colname="col5">(<inline-formula><mml:math id="M76" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M77" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col6">(<inline-formula><mml:math id="M78" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>, m)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">A1<inline-formula><mml:math id="M79" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">5</oasis:entry>
         <oasis:entry colname="col3">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">45</oasis:entry>
         <oasis:entry colname="col6">15</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A2</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">0</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A3</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">30</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A4</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">60</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A5</oasis:entry>
         <oasis:entry colname="col2">5</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4">0, 0.2, 0.4, 0.6, 0.8</oasis:entry>
         <oasis:entry colname="col5">45</oasis:entry>
         <oasis:entry colname="col6">15</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A6</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4">0.2</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A7</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">A8</oasis:entry>
         <oasis:entry colname="col2">25</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4">0.6</oasis:entry>
         <oasis:entry colname="col5">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15, 20, 30</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">B1<inline-formula><mml:math id="M80" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">5</oasis:entry>
         <oasis:entry colname="col3">0, 30, 45, 60, 90</oasis:entry>
         <oasis:entry colname="col4">0</oasis:entry>
         <oasis:entry colname="col5">null</oasis:entry>
         <oasis:entry colname="col6">null</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">B2</oasis:entry>
         <oasis:entry colname="col2">3</oasis:entry>
         <oasis:entry colname="col3">45</oasis:entry>
         <oasis:entry colname="col4">0.4</oasis:entry>
         <oasis:entry colname="col5">0</oasis:entry>
         <oasis:entry colname="col6">5, 10, 15</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">B3</oasis:entry>
         <oasis:entry colname="col2">5</oasis:entry>
         <oasis:entry colname="col3">90</oasis:entry>
         <oasis:entry colname="col4">0, 0.2, 0.4, 0.6, 0.8</oasis:entry>
         <oasis:entry colname="col5">null</oasis:entry>
         <oasis:entry colname="col6">null</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p id="d1e1262"><inline-formula><mml:math id="M73" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Simulation group “A” was designed for the metamodel modeling.
<inline-formula><mml:math id="M74" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> Simulation group “B” was designed for the detailed interpretations of sensitivity analysis results.</p></table-wrap-foot></table-wrap>

      <p id="d1e1653">In this study, the metamodels representing the objective function were
created using the 160 samples shown in <?xmltex \hack{\mbox\bgroup}?>Table 1<?xmltex \hack{\egroup}?>. In the metamodel modeling,
the variation range of the orientation (Or) was from
0 to 90<inline-formula><mml:math id="M81" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, the opening scale (Op) was from 0 to 0.8<inline-formula><mml:math id="M82" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, the azimuthal angle (<inline-formula><mml:math id="M83" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) was from 0 to 90<inline-formula><mml:math id="M84" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and the distance (<inline-formula><mml:math id="M85" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) was from 5 to 30 m.
The coefficient of determination (<inline-formula><mml:math id="M86" display="inline"><mml:mrow><mml:msup><mml:mi>R</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula>) of regression analysis in the GP
model was 0.88. At this accuracy, a total of 10 000 new simulation results
were obtained from random values in the specified ranges of the four input
variables for use in the subsequent sensitivity analysis.</p>
</sec>
<sec id="Ch1.S3.SS2">
  <label>3.2</label><title>Sensitivity analysis</title>
      <p id="d1e1721">Sensitivity analysis aims to understand the relative importance of uncertain
input variables to the model response (J. Zhang et al., 2021). As opposed to
local sensitivity analysis, GSA can be performed by an all-at-a-time method,
where output variations are induced by varying all input factors
simultaneously, and thus, the sensitivity of each factor considers the
direct influence of the factor, as well as the joint influence caused by the
factor interactions (Kim et al., 2019). GSA allows a ranking among the input
parameters to be established according to their influence on the variability
of the output. In this study, GSA was conducted to simultaneously consider
both the main and interaction effects of input parameters on debris flow
impact. A variance-based GSA (VBSA), also referred to as Sobol's indices, is
usually recommended.<?pagebreak page877?> This method is applicable over the whole space of
random input data and can also deal with nonlinear responses and measure the
effect of interactions in nonadditive systems (Saltelli et al., 2010). The
basic principle of Sobol's indices is that the variance of model output is
decomposed into fractions within a probabilistic framework that can be
attributed to inputs and sets of inputs (Sobol, 1993):
            <disp-formula id="Ch1.E3" content-type="numbered"><label>3</label><mml:math id="M87" display="block"><mml:mrow><mml:mi>V</mml:mi><mml:mo>=</mml:mo><mml:mi mathvariant="normal">Var</mml:mi><mml:mfenced open="[" close="]"><mml:mrow><mml:mi>f</mml:mi><mml:mfenced close=")" open="("><mml:mi>x</mml:mi></mml:mfenced></mml:mrow></mml:mfenced><mml:mo>=</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msub><mml:mi>V</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>≤</mml:mo><mml:mi>i</mml:mi><mml:mo>&lt;</mml:mo><mml:mi>j</mml:mi><mml:mo>≤</mml:mo><mml:mi>d</mml:mi></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mo>+</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:mi>d</mml:mi></mml:mrow></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where the partial variances are calculated as follows:
            <disp-formula id="Ch1.E4" content-type="numbered"><label>4</label><mml:math id="M88" display="block"><mml:mtable class="split" rowspacing="0.2ex" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub><mml:mo>=</mml:mo></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo movablelimits="false">∫</mml:mo><mml:msubsup><mml:mi>f</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:mfenced><mml:mi>p</mml:mi><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:mfenced><mml:mi mathvariant="normal">d</mml:mi><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>x</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub><mml:mo>,</mml:mo><mml:mspace linebreak="nobreak" width="1em"/><mml:mi>s</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:mi>d</mml:mi><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
          Sobol's indices are defined as the relative contribution of the partial
variances to the total variance following the decomposition in Eq. (1):
            <disp-formula id="Ch1.E5" content-type="numbered"><label>5</label><mml:math id="M89" display="block"><mml:mtable class="split" rowspacing="0.2ex" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow><mml:mi>V</mml:mi></mml:mfrac></mml:mstyle></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msub><mml:mi>V</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>≤</mml:mo><mml:mi>i</mml:mi><mml:mo>&lt;</mml:mo><mml:mi>j</mml:mi><mml:mo>≤</mml:mo><mml:mi>d</mml:mi></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mo>+</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:mi>d</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
          such that
            <disp-formula id="Ch1.E6" content-type="numbered"><label>6</label><mml:math id="M90" display="block"><mml:mrow><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msub><mml:mi>S</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:munder><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>≤</mml:mo><mml:mi>i</mml:mi><mml:mo>&lt;</mml:mo><mml:mi>j</mml:mi><mml:mo>≤</mml:mo><mml:mi>d</mml:mi></mml:mrow></mml:munder><mml:msub><mml:mi>S</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mo>+</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi>S</mml:mi><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:mi>d</mml:mi></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where the index <inline-formula><mml:math id="M91" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> measures the separate contribution of each variable
<inline-formula><mml:math id="M92" display="inline"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> to the output variance without interaction with any other inputs;
hence, <inline-formula><mml:math id="M93" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is commonly referred to as the first-order effect index or the
main effect index. The higher-order indices in Eq. (4) measure the
interactive contribution to the total variance. Using <inline-formula><mml:math id="M94" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M95" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mi>j</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> and
higher-order indices, we can therefore infer the impacts of each input
variable and the interaction of variables on the output variance (J. Zhang et
al., 2021). In this study, only the second-order effect index, reflecting
the interaction between every two factors, was considered. The total
contribution of variable <inline-formula><mml:math id="M96" display="inline"><mml:mi>i</mml:mi></mml:math></inline-formula> is as follows:
            <disp-formula id="Ch1.E7" content-type="numbered"><label>7</label><mml:math id="M97" display="block"><mml:mrow><mml:msubsup><mml:mi>S</mml:mi><mml:mi>i</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup><mml:mo>=</mml:mo><mml:munder><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mfenced close="}" open="{"><mml:mi>i</mml:mi></mml:mfenced><mml:mo>⊂</mml:mo><mml:mfenced close="}" open="{"><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:munder><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mrow><mml:msub><mml:mi>i</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>,</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>,</mml:mo><mml:msub><mml:mi>i</mml:mi><mml:mi>s</mml:mi></mml:msub></mml:mrow></mml:msub></mml:mrow><mml:mi>V</mml:mi></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          which measures the contributions of variable <inline-formula><mml:math id="M98" display="inline"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and its interactions to
the output variance. If the input <inline-formula><mml:math id="M99" display="inline"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> has a <inline-formula><mml:math id="M100" display="inline"><mml:mrow><mml:msubsup><mml:mi>S</mml:mi><mml:mi>i</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn></mml:mrow></mml:math></inline-formula>, then it
contributes 50 % of the overall variance of output. In Sobol's sensitivity
analysis, the input factors with a sensitivity index below 0.01 are usually
considered noninfluential to the output (Sarrazin et al., 2016). Unlike the
first-order indices,
            <disp-formula id="Ch1.E8" content-type="numbered"><label>8</label><mml:math id="M101" display="block"><mml:mrow><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>d</mml:mi></mml:munderover><mml:msubsup><mml:mi>S</mml:mi><mml:mi>i</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          because the interaction effect between, for example, <inline-formula><mml:math id="M102" display="inline"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M103" display="inline"><mml:mrow><mml:msub><mml:mi>x</mml:mi><mml:mi>j</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is
included in both <inline-formula><mml:math id="M104" display="inline"><mml:mrow><mml:msubsup><mml:mi>S</mml:mi><mml:mi>i</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M105" display="inline"><mml:mrow><mml:msubsup><mml:mi>S</mml:mi><mml:mi>j</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup></mml:mrow></mml:math></inline-formula>. The sum of <inline-formula><mml:math id="M106" display="inline"><mml:mrow><mml:msubsup><mml:mi>S</mml:mi><mml:mi>i</mml:mi><mml:mi mathvariant="normal">T</mml:mi></mml:msubsup></mml:mrow></mml:math></inline-formula> is
equal to 1 if and only if the model is purely additive without any
interaction effects.</p>
      <p id="d1e2492">In this study, Sobol's global sensitivity indices were calculated using the
SobolGSA model, a general purpose GUI-driven GSA software developed by Kucherenko and Zaccheus (2023; <uri>https://www.imperial.ac.uk/process-systems-engineering/research/free-software/sobolgsa-software/</uri>, last access: 23 February 2023).
SobolGSA evaluates the effect of a factor while all other factors are varied
as well, and thus,<?pagebreak page878?> it accounts for interactions between variables and does
not depend on the choice of a nominal point like local sensitivity analysis
methods. The set of available GSA techniques includes screening method- (the
Morris measure), variance- (Sobol's indices, FAST) and derivative-based
sensitivity measures. All techniques implemented in SobolGSA make use of
either quasi-Monte Carlo sampling based on Sobol's sequences or standard Monte
Carlo sampling (Sobol et al., 2011; Kucherenko et al., 2015).</p>
</sec>
</sec>
<sec id="Ch1.S4">
  <label>4</label><title>Results and discussion</title>
<sec id="Ch1.S4.SS1">
  <label>4.1</label><title>Results of global sensitivity analysis</title>
      <p id="d1e2514">Global sensitivity indices and total sensitivity indices for debris flow
impacts are listed in Table 2, and the main and total effects of each
parameter are expressed in Fig. 5. From the main effect indices, the peak
impact force is most sensitive to the azimuth angle, with a maximum value of
0.6303, which represents 63.03 % of the overall variance in the debris
flow peak impact loads. The most influential second-order effect index, with
a value of 0.1842, was obtained for the interaction between the azimuth
angle and the distance of the surrounding buildings. This result also
highlights the importance of the surrounding buildings' azimuth angle to the
debris flow impact over the distance's main effect index of 0.0095. The sums
of all main effect and second-order effect indices are 0.7648 and 0.2352,
respectively, indicating that single built environment parameters have a
more significant effect on the debris flow impact on a building.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T2"><?xmltex \currentcnt{2}?><label>Table 2</label><caption><p id="d1e2520">Global sensitivity indices and total sensitivity indices. The values in bold font are the maximum main effect and second-order effect indices.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="5">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="center"/>
     <oasis:colspec colnum="3" colname="col3" align="center"/>
     <oasis:colspec colnum="4" colname="col4" align="center"/>
     <oasis:colspec colnum="5" colname="col5" align="center"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Input variables</oasis:entry>
         <oasis:entry colname="col2">Or</oasis:entry>
         <oasis:entry colname="col3">Op</oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M107" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M108" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula></oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">Or</oasis:entry>
         <oasis:entry colname="col2">0.1200</oasis:entry>
         <oasis:entry colname="col3">0.0026</oasis:entry>
         <oasis:entry colname="col4">0.0346</oasis:entry>
         <oasis:entry colname="col5">0.0077</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Op</oasis:entry>
         <oasis:entry colname="col2">0.0026</oasis:entry>
         <oasis:entry colname="col3">0.0050</oasis:entry>
         <oasis:entry colname="col4">0.0040</oasis:entry>
         <oasis:entry colname="col5">0.0021</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M109" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">0.0346</oasis:entry>
         <oasis:entry colname="col3">0.0040</oasis:entry>
         <oasis:entry colname="col4"><bold>0.6303</bold></oasis:entry>
         <oasis:entry colname="col5"><bold>0.1842</bold></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M110" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">0.0077</oasis:entry>
         <oasis:entry colname="col3">0.0021</oasis:entry>
         <oasis:entry colname="col4">0.1842</oasis:entry>
         <oasis:entry colname="col5">0.0095</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Total effects</oasis:entry>
         <oasis:entry colname="col2">0.1649</oasis:entry>
         <oasis:entry colname="col3">0.0137</oasis:entry>
         <oasis:entry colname="col4">0.8531</oasis:entry>
         <oasis:entry colname="col5">0.2035</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5"><?xmltex \currentcnt{5}?><?xmltex \def\figurename{Figure}?><label>Figure 5</label><caption><p id="d1e2677">Main and total effects of parameters for debris flow peak impact
forces.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f05.jpg"/>

        </fig>

      <p id="d1e2687">From the total effect indices, on the other hand, the importance of the
built environment parameters to the debris flow impact responses is ranked
as follows: azimuth angle (<inline-formula><mml:math id="M111" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) <inline-formula><mml:math id="M112" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> distance
(<inline-formula><mml:math id="M113" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) <inline-formula><mml:math id="M114" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> orientation (Or) <inline-formula><mml:math id="M115" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> opening scale (Op), and their total effect
indices are 0.8531, 0.2035, 0.1649 and 0.0137, respectively. The sum of the
main effects of the target building's properties (Or <inline-formula><mml:math id="M116" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> Op) is 0.1786 and that of the surrounding buildings' properties (<inline-formula><mml:math id="M117" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M118" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> <inline-formula><mml:math id="M119" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) is 1.0566,
indicating that the surrounding buildings' properties are more significant
than the target building's properties on the peak impact forces.</p>
      <p id="d1e2754"><?xmltex \hack{\newpage}?>Finally, it is concluded that the azimuth angle and distance of the
surrounding buildings and the target building's orientation are the key
factors and must be carefully considered in the assessment of building
vulnerability to debris flow impacts. It is highly recommended to further
study the effect of the surrounding buildings' azimuth angles. Although the
scale of building openings indeed has a nonsignificant effect on debris flow
impacts in this study, the other features of building openings, such as
their location, height and structure, should be discussed in more depth.</p>
</sec>
<sec id="Ch1.S4.SS2">
  <label>4.2</label><title>Effect of the surrounding buildings' azimuthal angles</title>
      <p id="d1e2766">As shown in Fig. 6, the peak impact forces of the debris flow change with
the increasing azimuth angles in the simulation scenarios at an orientation
of 90<inline-formula><mml:math id="M120" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, an opening scale of 0.4 and a distance of 5 m
(Or90-Op0.4-<inline-formula><mml:math id="M121" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M122" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, where <inline-formula><mml:math id="M123" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula> represents a variable). The variations in the peak impact forces are calculated with the background value of 3717 kN from the scenario with an orientation of 90<inline-formula><mml:math id="M124" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, opening scale of 0.4 and no surrounding buildings (Or90-Op0.4-<inline-formula><mml:math id="M125" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M126" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null,
where null means the value is not relevant). The azimuth angles have
different kinds of effects on debris flow impacts, as shown in the different
colored zones in Fig. 6:
<list list-type="order"><list-item>
      <p id="d1e2828"><italic>Shielding effect</italic>. In the cases of azimuth angles of 0<inline-formula><mml:math id="M127" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
(Or90-Op0.4-<inline-formula><mml:math id="M128" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M129" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5) and 30<inline-formula><mml:math id="M130" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or90-Op0.4-<inline-formula><mml:math id="M131" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M132" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5),
the peak impact forces are only 796 and 1193 kN, and the corresponding
variations (<inline-formula><mml:math id="M133" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>F</mml:mi></mml:mrow></mml:math></inline-formula>) are <inline-formula><mml:math id="M134" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>78.58 % and <inline-formula><mml:math id="M135" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>67.90 %, respectively, which are located in the blue shielding effect region
(<inline-formula><mml:math id="M136" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>F</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M137" display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> <inline-formula><mml:math id="M138" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>10 %) in Fig. 6. It is indicated that the target building is protected
effectively in a shielding area produced by the surrounding buildings. This
result is consistent with previous case studies wherein some representative
catastrophic debris flow events were observed. In the Zhouqu debris flow
event<?pagebreak page879?> shown in Fig. 7, which occurred in the province of Gansu in northwestern
China, on 7 August 2010, building B, next to the extensively damaged
building A, suffered no damage apart from its first story being buried (Hu
et al., 2012). Similarly, in the Qipan gully debris flow case (Zeng et al.,
2015), which occurred in the city of Wenchuan in southwestern China during
rainstorms on 11 July 2013, building B, shielding protected from the
completely damaged building A, was exposed to only slight damage, as shown
in region I of Fig. 8. As shown in Fig. 9, a deflection wall was designed
following the principles of the shielding effect and can be repeatedly used
to protect an entire building ensemble from gravitational mass movements,
such as the snow avalanches, in the mountain areas of Austria (Holub et al., 2012). This design of local protection can provide an effective reference for debris flow mitigation.</p></list-item><list-item>
      <p id="d1e2930"><italic>Canalization effect</italic>. As reported by Sturm et al. (2018a) through flume
tests, the existence of surrounding buildings may narrow the flow path and
even redirect debris flows, leading to an increasing process intensity
toward other buildings (Gao et al., 2017). In these numerical simulations,
the azimuth angle of 45<inline-formula><mml:math id="M139" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or90-Op0.4-<inline-formula><mml:math id="M140" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M141" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5)
has the most significant canalization effect on the target building and
produces the steepest rise in the peak impact force, with 29.14 % growth to a maximum  value of 4800 kN, as shown in the orange region (<inline-formula><mml:math id="M142" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>F</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M143" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 10 %) of Fig. 6. As shown in region IV of Fig. 8, building I was exposed to extensive damage in the Qipan gully debris flow partly because of the canalization effect induced by surrounding building J.</p></list-item><list-item>
      <p id="d1e2976"><italic>Noneffect</italic>. The peak impact forces in the cases of azimuth angles of
60<inline-formula><mml:math id="M144" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or90-Op0.4-<inline-formula><mml:math id="M145" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>60-<inline-formula><mml:math id="M146" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5) and 90<inline-formula><mml:math id="M147" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
(Or90-Op0.4-<inline-formula><mml:math id="M148" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>90-<inline-formula><mml:math id="M149" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5) are 3584 and 3725 kN, respectively, close to the background value (3717 kN),
and the corresponding variations are also close to 0, located in the green
region (<inline-formula><mml:math id="M150" display="inline"><mml:mo lspace="0mm">-</mml:mo></mml:math></inline-formula>10 % <inline-formula><mml:math id="M151" display="inline"><mml:mo>≤</mml:mo></mml:math></inline-formula> <inline-formula><mml:math id="M152" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>F</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M153" display="inline"><mml:mo>≤</mml:mo></mml:math></inline-formula> 10 %) of Fig. 6. This indicates
that there are very small or even negligible effects on the impact loads of
the target building. It is important to highlight that the shielding effect
has the greatest influence on debris flow impact loads, because this effect
yields the maximum variation in peak impact forces.</p></list-item></list></p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6"><?xmltex \currentcnt{6}?><?xmltex \def\figurename{Figure}?><label>Figure 6</label><caption><p id="d1e3061">Variations of peak impact forces with increasing azimuth angles in the
scenarios of the orientation of 90<inline-formula><mml:math id="M154" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and the opening scale of 0.4 and distance of 5 m
(Or90-Op0.4-<inline-formula><mml:math id="M155" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M156" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5).</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f06.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7"><?xmltex \currentcnt{7}?><?xmltex \def\figurename{Figure}?><label>Figure 7</label><caption><p id="d1e3098">Distribution of damaged buildings in the Zhouqu debris flow event.
Orthophoto map is from DigitalGlobe's WorldView-2 satellite on 22 October
2010 published by NASA (ref: <uri>https://earthobservatory.nasa.gov/images/45329/landslide-in-zhouqu-china</uri>, last access: 23 February 2023); the aerial photo is referred from the website of <uri>http://slide.news.sina.com.cn/c/slide_1_5039_12703.html</uri> (last access: 23 February 2023; Tang et al., 2011).</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f07.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><?xmltex \currentcnt{8}?><?xmltex \def\figurename{Figure}?><label>Figure 8</label><caption><p id="d1e3116">Distribution of damaged buildings in the Qipan gully debris flow
event. Orthophoto map is from the Basic Geographic Information Center of
the province of Sichuan, China, 21 July 2013.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f08.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F9"><?xmltex \currentcnt{9}?><?xmltex \def\figurename{Figure}?><label>Figure 9</label><caption><p id="d1e3127">A deflection wall used to protect an entire building ensemble from
the impact of medium-magnitude events (Galtur Tschafein, Austria) (Holub et
al., 2012).</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f09.jpg"/>

        </fig>

</sec>
<sec id="Ch1.S4.SS3">
  <label>4.3</label><title>Effect of the distance to the surrounding buildings</title>
      <p id="d1e3144">As shown in Fig. 10, the variations in peak impact forces change with the
surrounding buildings' distances in conjunction with the influences of
azimuth angles. The scenario of the orientation of 90<inline-formula><mml:math id="M157" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and opening
of 0.4 (Or90-Op0.4-<inline-formula><mml:math id="M158" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M159" display="inline"><mml:mrow><mml:mi>D</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>) is taken as an example, and the background value (Or90-Op0.4-<inline-formula><mml:math id="M160" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M161" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null)
is still 3717 kN. According to the results of the sensitivity analysis, the
most significant second-order effect comes from the interaction between the
azimuth angle and distance, which can be divided into an amplification of
the shielding effect or a reduction in the canalization effect, as shown in
Fig. 10.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F10" specific-use="star"><?xmltex \currentcnt{10}?><?xmltex \def\figurename{Figure}?><label>Figure 10</label><caption><p id="d1e3192">Peak impact forces change with the surroundings' distances under the
influence of azimuth angles in the scenarios of the orientation of 90<inline-formula><mml:math id="M162" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
and the opening scale of 0.4 (Or90-Op0.4-<inline-formula><mml:math id="M163" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M164" display="inline"><mml:mrow><mml:mi>D</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>).</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f10.jpg"/>

        </fig>

      <p id="d1e3230"><?xmltex \hack{\newpage}?><list list-type="order">
            <list-item>

      <p id="d1e3236"><italic>Amplification of the shielding effect</italic>. The peak impact forces are found to be reduced gradually with increasing surrounding building distance in the case of an azimuth angle of 0<inline-formula><mml:math id="M165" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
(Or90-Op0.4-<inline-formula><mml:math id="M166" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M167" display="inline"><mml:mrow><mml:mi>D</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula>), with a 5 m distance yielding 796 kN and a 30 m distance yielding 467 kN, and the corresponding variations in peak impact forces are approximately <inline-formula><mml:math id="M168" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>78.58 % and <inline-formula><mml:math id="M169" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>87.44 %. The shielding effects at an azimuth angle of 0<inline-formula><mml:math id="M170" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> are amplified with increasing surrounding distance. This process occurs because there is a broader shielding area further downstream of the surrounding building when the debris flow path is separated by an obstacle at a fixed angle of spread, as shown in Fig. 11. Furthermore, there
is likely a small-scale debris flow conflux zone close to the surrounding
building, as shown in the red zone of Fig. 11. Buildings upstream,
therefore, may suffer from a higher impact load in the same debris flow
shielding area. As shown in region III of Fig. 8, the lower a building's
damage degree, the further away the completely damaged building D is in the
back shielding area. Building E, next to building D, is exposed to moderate
damage, and other shielding-protected buildings, such as buildings F, G and
H, experience only slight damage from lateral abrasion and accumulation.
However, the amplified shielding effect inevitably disappears further
downstream due to the confluence of debris flow runoff. The range of the
shielding area mainly depends on the debris flow properties, especially the
friction coefficient and dynamic viscosity (Liang et al., 2021).<?pagebreak page881?> Further
investigation of the effective shielding-protection area is needed.</p>
            </list-item>
            <list-item>

      <p id="d1e3294"><italic>Reduction in the canalization effect</italic>. The canalization effect mainly
occurs under a surrounding building at an azimuth angle of 45<inline-formula><mml:math id="M171" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, as
mentioned above; however, this kind of effect could be lessened under the
influence of the surrounding buildings' distances. As shown by the red line
in Fig. 10, the maximum peak impact force under an azimuth angle of
45<inline-formula><mml:math id="M172" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, with a value of 4800 kN, appears with a distance of 5 m
(Or90-Op0.4-<inline-formula><mml:math id="M173" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M174" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5). Then, the peak impact forces decrease rapidly with greater distances, especially in the distance range of less than 15 m. The peak impact force at a distance of 15 m (Or90-Op0.4-<inline-formula><mml:math id="M175" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M176" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>15)
is reduced to 3462 kN, which is very close to the background value (3717 kN). It is indicated that the canalization effect under an azimuth angle of 45<inline-formula><mml:math id="M177" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> may have vanished completely at this point. As shown in the computational results at 8.0 s in Fig. 12, the increase in flow velocity in
the narrowed flow paths due to building blockage decreases with increasing
surrounding building distances. The increased-velocity debris flows, on the
other hand, tend to flow away from the target building in the cases of
greater surrounding building distances. Therefore, the variations in peak
impact forces are close to 0 due to the lower flow velocity and fewer
intruding materials in the scenarios of surrounding building distances
beyond 15 m. In general, a greater distance results in a lower impact force.</p>
            </list-item>
          </list></p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F11"><?xmltex \currentcnt{11}?><?xmltex \def\figurename{Figure}?><label>Figure 11</label><caption><p id="d1e3360">There is the lower debris flow intensities further away
surrounding building within a shielding area, in the scenario of
Or90-Op0.4-<inline-formula><mml:math id="M178" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M179" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>30 at a simulation time of 8.0 s. The local debris flow conflux is delineated with the dotted red line (the snapshot has been rotated 30<inline-formula><mml:math id="M180" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> counterclockwise along the <inline-formula><mml:math id="M181" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula> axis, similarly
hereinafter).</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f11.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F12" specific-use="star"><?xmltex \currentcnt{12}?><?xmltex \def\figurename{Figure}?><label>Figure 12</label><caption><p id="d1e3401">Snapshots for debris flow intensities in the scenarios of
Or90-Op0.4-<inline-formula><mml:math id="M182" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M183" display="inline"><mml:mrow><mml:mi>D</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula> at a simulation time of 8.0 s. Panel <bold>(a)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M184" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M185" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, <bold>(b)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M186" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M187" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>10, <bold>(c)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M188" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M189" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>15, <bold>(d)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M190" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M191" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>20 and <bold>(e)</bold> is the case of
Or90-Op0.4-<inline-formula><mml:math id="M192" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M193" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>30.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f12.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F13" specific-use="star"><?xmltex \currentcnt{13}?><?xmltex \def\figurename{Figure}?><label>Figure 13</label><caption><p id="d1e3516">Snapshots for debris flow intensities in the scenarios of
Or90-Op0.4-<inline-formula><mml:math id="M194" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M195" display="inline"><mml:mrow><mml:mi>D</mml:mi><mml:mi>x</mml:mi></mml:mrow></mml:math></inline-formula> at a simulation time of 8.0 s. Panel <bold>(a)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M196" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M197" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, <bold>(b)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M198" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M199" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>10, <bold>(c)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M200" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M201" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>15, <bold>(d)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M202" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M203" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>20 and <bold>(e)</bold> is the case of
Or90-Op0.4-<inline-formula><mml:math id="M204" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M205" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>30.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f13.jpg"/>

        </fig>

      <p id="d1e3629">​​​​​​​A smaller surrounding building distance, however, does not necessarily indicate a larger impact force. With surrounding building distances of 5 and 10 m, impact force shielding effects occur under the condition of an azimuth angle of 30<inline-formula><mml:math id="M206" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or90-Op0.4-<inline-formula><mml:math id="M207" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M208" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5
and Or90-Op0.4-<inline-formula><mml:math id="M209" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M210" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>10), as shown in Fig. 13, and the corresponding variations in peak impact loads are <inline-formula><mml:math id="M211" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>67.90 % and <inline-formula><mml:math id="M212" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>22.03 %, respectively. The width of the narrowed flow
path, which is determined by the factors of the azimuth angle and
surrounding building distance, could account for this fact. The flow paths
are so narrow, with widths of 1.6 and 6.6 m, respectively, like
bottlenecks, that not much flow passes through them, as shown in Fig. 13a
and b. Thereafter, the canalization effect occurs at distances beyond
15 m and reduces and even disappears<?pagebreak page882?> gradually with increasing surrounding
building distance and the corresponding wider flow paths. It is found that
the ratio of the width of the narrowed flow path to the length of the target
building has a significant effect on the increase in impact force. The
largest peak impact force is most likely to be found under a ratio of
approximately one, for example, the ratios of 0.8 in the case of
Or90-Op0.4-<inline-formula><mml:math id="M213" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>45-<inline-formula><mml:math id="M214" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5 (Fig. 12a) and 1.1 of Or90-Op0.4-<inline-formula><mml:math id="M215" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>30-<inline-formula><mml:math id="M216" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>20
(Fig. 13d).</p>
</sec>
<sec id="Ch1.S4.SS4">
  <label>4.4</label><title>Effect of the orientation</title>
<sec id="Ch1.S4.SS4.SSS1">
  <label>4.4.1</label><title>Single-factor analysis of orientation</title>
      <?pagebreak page883?><p id="d1e3727">As shown in Fig. 14, the peak impact forces of debris flows are ordered as
follows: Or90 <inline-formula><mml:math id="M217" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> Or60 <inline-formula><mml:math id="M218" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> Or0 <inline-formula><mml:math id="M219" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> Or45 <inline-formula><mml:math id="M220" display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> Or30, and the corresponding values are 3560, 2591, 2334, 1917 and 1912 kN, respectively, when only the target building's orientation is considered
(Orx-Op0-<inline-formula><mml:math id="M221" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M222" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null).
It is generally accepted that the impact load of a debris flow is a
comprehensive outcome from many characteristic parameters, including the
debris flow density, velocity, impact contact area and approaching angle
(Liu et al., 2021). It is assumed that the debris flow density is constant
in the computational process of impact forces in the FLOW-3D model.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F14"><?xmltex \currentcnt{14}?><?xmltex \def\figurename{Figure}?><label>Figure 14</label><caption><p id="d1e3775">Peak impact forces change with the target building's orientations in
the scenarios of no openings and no surroundings
(Orx-Op0-<inline-formula><mml:math id="M223" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M224" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null).</p></caption>
            <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f14.jpg"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F15" specific-use="star"><?xmltex \currentcnt{15}?><?xmltex \def\figurename{Figure}?><label>Figure 15</label><caption><p id="d1e3800">Snapshots for debris flow intensities in the scenarios of
Orx-Op0-<inline-formula><mml:math id="M225" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M226" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null at a simulation time of 8.0 s. Panel <bold>(a)</bold> is the case of Or0-Op0-<inline-formula><mml:math id="M227" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M228" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null, <bold>(b)</bold> is the case of Or30-Op0-<inline-formula><mml:math id="M229" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M230" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null, <bold>(c)</bold> is the case of Or45-Op0-<inline-formula><mml:math id="M231" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M232" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null, <bold>(d)</bold> is the case of Or60-Op0-<inline-formula><mml:math id="M233" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M234" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null and <bold>(e)</bold> is the case of
Or90-Op0-<inline-formula><mml:math id="M235" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M236" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null.</p></caption>
            <?xmltex \igopts{width=384.112205pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f15.jpg"/>

          </fig>

      <p id="d1e3911">The impact contact area, a product of the wall length and effective height,
where the latter is the minimum value between the wall height and flow
depth, can be used to explain the debris flow impact responses in the case
of orientations of 0<inline-formula><mml:math id="M237" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or0-Op0-<inline-formula><mml:math id="M238" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M239" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null) and 90<inline-formula><mml:math id="M240" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
(Or90-Op0-<inline-formula><mml:math id="M241" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M242" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null).
In the simulations shown in Fig. 15a and e, the single wall element,
wall B or wall A, is vertically impacted by debris flows, and the surging
flows go beyond the wall height. The length of the impacted wall elements,
therefore, should contribute to the difference in the peak impact pressures.
The mainly impacted wall element in the orientation of 90<inline-formula><mml:math id="M243" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> – wall A of 15 m – is obviously longer than that of the orientation of 0<inline-formula><mml:math id="M244" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, wall B of 10 m. A larger contact area results in a greater impact force.</p>
      <p id="d1e3979">Walls A and B are simultaneously exposed to debris flows in the orientations
of 30, 45 and 60<inline-formula><mml:math id="M245" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, as shown in Fig. 15b–d.
In these cases, the debris flow impact loads, to a large extent, are
dominated by the approaching angle, which is defined here as the general,
temporally independent angle of the wall element to the main flow path, with
a range of 0<inline-formula><mml:math id="M246" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (parallel) to 90<inline-formula><mml:math id="M247" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (vertical). Generally,
there are higher flow velocities and lower surge flow depths in the cases of
smaller approaching angles and vice versa. The highest flow depth occurs in
the neighborhood of wall A, the longest wall of the target building, in the
scenario with an orientation of 60<inline-formula><mml:math id="M248" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or60-Op0-<inline-formula><mml:math id="M249" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M250" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null),
as shown in Fig. 15d. In contrast, the lowest flow depth appears near wall
A, with an orientation of 30<inline-formula><mml:math id="M251" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or30-Op0-<inline-formula><mml:math id="M252" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M253" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null),
as shown in Fig. 15b. This could be the main reason why the impact force of the target building with 60<inline-formula><mml:math id="M254" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> orientation is larger than the one of 30<inline-formula><mml:math id="M255" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> orientation. However, even so, better migration performances, such as lower
impact loads and larger shielding areas, are produced in these cases than in
the case with an orientation of 90<inline-formula><mml:math id="M256" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. Similar to this idea, a
splitting wedge, with a triangular shape and two downslope-directed sides,
was constructed at the process-oriented side of an exposed building to
protect against snow avalanches in the Swiss Alps, as shown in Fig. 16. It
was confirmed that splitting wedges, with this very distinctive shape, were
considerably effective in maintaining its stability and offering a larger
protected zone for the other neighboring buildings. It also provides a good
model for building protection design in debris-flow-prone areas. The main
criterion for the effective operation of such a structure is avoiding the
highest flow depth – the maximum approaching angle – appearing near the
longest wall element.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F16"><?xmltex \currentcnt{16}?><?xmltex \def\figurename{Figure}?><label>Figure 16</label><caption><p id="d1e4086">Splitting wedge directly connected to the exposed object (Davos
Frauenkirch, Switzerland) (Holub et al., 2012).</p></caption>
            <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f16.jpg"/>

          </fig>

      <p id="d1e4095">Last but not least, flip-though impacts, caused by the backwater effect,
which is a special phenomenon when debris flow hits a barrier wall, runs up,
bounces backward, blocks and converges with the remaining debris (Takahashi,
2007; Song et al., 2021), contributing greatly to the peak impact forces of
orientations 0<inline-formula><mml:math id="M257" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (Or0-Op0-<inline-formula><mml:math id="M258" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M259" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null) and 90<inline-formula><mml:math id="M260" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
(Or90-Op0-<inline-formula><mml:math id="M261" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M262" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null),
as shown in Fig. 17. The impact forces with an orientation of 0<inline-formula><mml:math id="M263" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>
reach their peak when the debris flow first collides with the wall and runs
up. The peak impact load with an orientation of 90<inline-formula><mml:math id="M264" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> comes from the
secondary waves overtaking the flow front, after the flow bounces off the
wall, collides and converges with the flow approaching from behind (Iverson
et al., 2010; Choi et al., 2018).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F17"><?xmltex \currentcnt{17}?><?xmltex \def\figurename{Figure}?><label>Figure 17</label><caption><p id="d1e4165">Impact forces time history with changing orientations in the
scenarios of Orx-Op0-<inline-formula><mml:math id="M265" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M266" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null after a simulation time of 4.0 s.</p></caption>
            <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f17.jpg"/>

          </fig>

</sec>
<sec id="Ch1.S4.SS4.SSS2">
  <label>4.4.2</label><title>Interaction between orientation and surroundings</title>
      <p id="d1e4196">The single-factor analysis of orientation explained why the buildings with
orientations of 30, 45 and 60<inline-formula><mml:math id="M267" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> have better
migration effects. This knowledge has to be reconsidered, however, when the
effect overlaps with the surrounding buildings' shielding effects. It is
found that buildings with orientations of 30, 45 and
60<inline-formula><mml:math id="M268" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> are more likely to be damaged by debris flows within a
shielding area. For instance, the maximum peak impact forces with
surrounding buildings' distances of 5 m (Or60-Op0.4-<inline-formula><mml:math id="M269" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M270" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5), 10 m
(Or60-Op0.4-<inline-formula><mml:math id="M271" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M272" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>10) and 15 m (Or60-Op0.4-<inline-formula><mml:math id="M273" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M274" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>15),
as shown in Fig. 18, are different from those of the single-factor analysis
of orientation. The protruding parts of the target building caused by the
changing orientations significantly contribute to the increase in impact
forces (Hu et al., 2012; Zeng et al., 2015). A larger protruding portion of
a building results in a greater probability of being exposed and
corresponding larger impact forces. The largest protruding areas are exposed
to debris flows at an orientation of 60<inline-formula><mml:math id="M275" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, as shown in Fig. 19d-1
and d-2). This can be confirmed by Fig. 8d. Although the main
structure of building E is in the shielding area of building D, its
protruding part is still completely destroyed by debris flows.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F18"><?xmltex \currentcnt{18}?><?xmltex \def\figurename{Figure}?><label>Figure 18</label><caption><p id="d1e4271">Peak impact forces change with the target building's orientations
under the shielding effect. The orange line shows the case of
Orx-Op0.4-<inline-formula><mml:math id="M276" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M277" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, the blue line shows the case of Orx-Op0.4-<inline-formula><mml:math id="M278" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M279" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>10 and the gray line shows the case of Orx-Op0.4-<inline-formula><mml:math id="M280" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M281" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>15.</p></caption>
            <?xmltex \igopts{width=213.395669pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f18.jpg"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F19" specific-use="star"><?xmltex \currentcnt{19}?><?xmltex \def\figurename{Figure}?><label>Figure 19</label><caption><p id="d1e4325">Snapshots for debris flow intensities in scenarios of
Orx-Op0.4-<inline-formula><mml:math id="M282" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M283" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5 at a simulation time of 8.0 s. Panel <bold>(a)</bold> is the case of Or0-Op0.4-<inline-formula><mml:math id="M284" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M285" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, <bold>(b)</bold> is the case of Or30-Op0.4-<inline-formula><mml:math id="M286" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M287" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, <bold>(c)</bold> is the case of Or45-Op0.4-<inline-formula><mml:math id="M288" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M289" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5, <bold>(d)</bold> is the case of Or60-Op0.4-<inline-formula><mml:math id="M290" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M291" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5 and <bold>(e)</bold> is the case of Or90-Op0.4-<inline-formula><mml:math id="M292" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>0-<inline-formula><mml:math id="M293" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>5. Panels <bold>(d-1)</bold> and <bold>(d-2)</bold> show in detail that the protruding portions of the target
building are exposed to debris flow.</p></caption>
            <?xmltex \igopts{width=423.946063pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f19.jpg"/>

          </fig>

<?xmltex \hack{\newpage}?>
</sec>
</sec>
<?pagebreak page884?><sec id="Ch1.S4.SS5">
  <label>4.5</label><title>Effect of the opening scale</title>
      <p id="d1e4454">According to the sensitivity analysis results, the opening scale is the
least important factor for debris flow impacts, as it yields the minimum
first-order effect index, 0.0050, and the minimum total effect index,
0.0137. From the results with an orientation of 90<inline-formula><mml:math id="M294" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and no
surrounding buildings (Or90-Opx-<inline-formula><mml:math id="M295" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M296" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null),
shown in Fig. 20, the peak impact forces of the target building change very
slightly with increasing opening scale. There is a maximum peak impact force
of 3945 kN in the case of openings with a scale of 0.8
(Or90-Op0.8-<inline-formula><mml:math id="M297" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M298" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null), which is approximately 15.38 % larger than the 3419 kN of openings with a scale of 0.2 (Or90-Op0.2-<inline-formula><mml:math id="M299" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M300" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null).
Interestingly, the impact responses of the target building are different
with different opening scales. Specifically, there are smaller impact forces
in the cases of larger opening scales when only wall A of the target
building is impacted, that is, in the early stage of debris flow impact from
5.3 to 6.2 s, as shown in Fig. 21. In this stage, the maximum impact
pressure of 865 kN of an opening scale of 0.8 is approximately half of the 1618 kN of an opening scale of 0.2; this is due to the difference in the effective
impacted<?pagebreak page885?> areas. From this perspective, the mitigation performance of single
wall elements with more openings is proven (Mazzorana et al., 2014; Gems et
al., 2016). Thereafter, the impact load of the overall building increases
rapidly following the abundant intrusion of materials through openings after
6.2 s, as shown in Fig. 21. Due to the greater accessibility and higher flow
velocity, there is faster growth in impact pressure in the scenarios with
the larger opening scales. Finally, after the two above-described impact
stages are combined, there are only slight differences between multiple
scales of openings in terms of peak impact forces. This indicates that the
mitigation function of openings for the whole building is very limited if
the time for material intrusion is sufficient.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F20"><?xmltex \currentcnt{20}?><?xmltex \def\figurename{Figure}?><label>Figure 20</label><caption><p id="d1e4511">Peak impact forces change with the target building's opening scale in
the scenarios of Or90-Opx-<inline-formula><mml:math id="M301" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M302" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f20.jpg"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F21" specific-use="star"><?xmltex \currentcnt{21}?><?xmltex \def\figurename{Figure}?><label>Figure 21</label><caption><p id="d1e4536">Impact force time history with changing opening scales in the
scenarios of Or90-Opx-<inline-formula><mml:math id="M303" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>null-<inline-formula><mml:math id="M304" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>null after a simulation time of 4.0 s.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/23/871/2023/nhess-23-871-2023-f21.jpg"/>

        </fig>

</sec>
</sec>
<sec id="Ch1.S5" sec-type="conclusions">
  <label>5</label><title>Conclusions and outlook</title>
      <p id="d1e4569">The effects of representative built environment parameters on the debris
flow impacts on a whole building were explored through FLOW-3D simulations
after validation with a published dam-break experiment. Four parameters
influencing the impact responses of the whole building induced by debris
flows were considered in this study: the orientation and opening scale of
the target building and the azimuthal angle and distance of the surrounding
buildings. The debris flow impact performance was evaluated using the
measurable indicator of the peak impact force acting on the overall
building. It is important to stress that the presented study and results
were subject to a number of assumptions and limitations: (1) the type of
debris flow was limited as mudflow or viscous debris flow, the solid was
assumed to be mixed well with the fluid phase, and the sediment deposition
was not considered; (2) the deposition fan was simplified for the modeling,
for example, the drainage channel and bed scour had been ignored; (3) the
inflow condition was different with the realistic debris flow hydrograph,
the discharge was fixed as 500 m<inline-formula><mml:math id="M305" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> s<inline-formula><mml:math id="M306" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and duration was limited to
5s, and the peak impact force was treated as the maximum value within the
computation time of 15 s. Finally, the main outcomes of the study may be
outlined as follows:
<list list-type="order"><list-item>
      <p id="d1e4595">The GSA based on metamodels with 160 cases reveals that the ranking of the importance of the built environment parameters on debris flow impacts from the results of total effect indices is azimuth angle (<inline-formula><mml:math id="M307" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) <inline-formula><mml:math id="M308" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> distance (<inline-formula><mml:math id="M309" display="inline"><mml:mi>D</mml:mi></mml:math></inline-formula>) <inline-formula><mml:math id="M310" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> orientation (Or) <inline-formula><mml:math id="M311" display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> opening scale (Op). The azimuth angle of the surrounding buildings alone
contributes to 63.03 % of the overall variance of the debris flow peak
impact load. The properties of the surrounding buildings, including the
azimuth angle and distance, are found to have a more significant influence
on the peak impact forces.</p></list-item><list-item>
      <p id="d1e4634">The azimuth angle has a shielding or canalization effect on debris flow
impacts. The shielding effect, a form of reducing impact pressures, mainly
appears in the scenarios with a surrounding building azimuth angle of
0<inline-formula><mml:math id="M312" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. The canalization effect, caused by narrowing and redirecting
of the flow path, is a form of increasing impact forces and occurs at an
azimuth angle of 45<inline-formula><mml:math id="M313" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. A deflection wall for building protection
is recommended, as this provides a shielding effect. The interaction between the azimuth angle and distance can be divided into the amplification of the shielding effect and the reduction in the canalization effect. The former is where buildings are less impacted with a limited increase in distance within a shielding area. Further investigation on the effective area of shielding protection is needed. The latter is where the peak impact force induced by the canalization effect decreases rapidly with a greater distance. The ratio
of the width of the narrowed flow path to the length of the target building
has a significant effect on the variation in the impact forces, and the
maximum peak impact pressure appears at a ratio of approximately one.</p></list-item><list-item>
      <p id="d1e4656">These parameters involving the building's impact response, including the impact contact area, approaching angle and flip-though impact, contribute to
the debris flow impact forces when only the orientation factor is
considered. A splitting wedge is recommended for an effective design,
mitigating the threat of debris flow, and the main criterion is avoiding the highest flow depth – the maximum approaching angle – appearing near the longest wall element. The buildings with orientations of 30,
45 and 60<inline-formula><mml:math id="M314" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> are more likely to be impacted by debris
flows in a shielding area due to the exposed protruding parts produced by
the building's rotations. As far as openings are concerned, although the
mitigation performance of this single wall element has been proven,<?pagebreak page886?> a
limited effect on the whole building is observed when there is enough time
for material intrusion.</p></list-item></list>
It is obvious that the quantitative descriptions about the interactions
between the built environment and impact forces can be useful to the built
environment improvement and local adaptation measures for the impact force
reduction, which are assumed as a low-cost and efficient approach for
mitigating the building's structural damages. And more significantly, the
present paper has extended the knowledge about the influence factors on
debris flow intensity. It is demonstrated that some artificial building
factors can not be ignored, except for the natural environments, in deciding
the spatial pattern of the process intensity. Further research about
their relative importance with the 3-D numerical simulation and sensitivity
analysis can promote the relative intensity evaluation of the building,
especially in terms of the indicator selection and weighting, which may open
a future topic of the debris flow hazard assessment. For the building
vulnerability assessment, the indicators can be mainly divided into two
kinds: the exterior process intensity and interior building resistance. The
process intensity, for example the flow depth, velocity, impact force or the
other proxy, was assumed absolutely necessary, either in the curve-based
approach or the indicator-based approach (Martinez-Carvajal et al., 2018).
From the current literature, however, there is some confusion in selecting
the surrounding factors and process intensity indicator. To be specific,
some surrounding factors or also called protection factors, including the
surrounding buildings, building row, wall around the building, natural barriers
and so on, were still selected when the debris flow intensity had been
indirectly considered (Dall'Osso et al., 2009, 2016;
Papathoma-Köhle et al., 2019). These indicators should be independent
of each other theoretically. From the views of the present paper, these surrounding factors have a significant influence on the process intensity. Therefore, the process intensity should be
exclusive with the surrounding factors. The building feature factors are
mainly considered to be acted on the building resistance, including the
material, structure, number of stories, foundation strength and so on.
However, it is not hard to find that some building indicators, for example
the orientation, shape and openings, can rebuild the process intensity. As a
result, the effect of the representative building feature indicators on the
building vulnerability needs an in-depth discussion in future. Last but
not least, a more universal, robust index may be developed using the
numerical simulation approach, which can improve the locality limits
resulting from the empirical data, to some extent.</p>
</sec>

      
      </body>
    <back><notes notes-type="codeavailability"><title>Code availability</title>

      <p id="d1e4673">The sensitivity analysis in this study is executed by the SobolGSA model (<uri>https://www.imperial.ac.uk/process-systems-engineering/research/free-software/sobolgsa-software/</uri>, upon registration; Kucherenko and Zaccheus, 2023).</p>
  </notes><notes notes-type="dataavailability"><title>Data availability</title>

      <p id="d1e4682">All data used during the study are available from the corresponding author by request.</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d1e4688">XH and ZZ contributed to the original idea and study design. XH, ZZ and GX participated in the field survey. XH and ZZ conducted the simulation and analysis. XH wrote the original manuscript, and ZZ and GX provided comments and revised the manuscript. All the co-authors contributed to scientific interpretations of the results.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <p id="d1e4694">The contact author has declared that none of the authors has any competing interests.</p>
  </notes><notes notes-type="disclaimer"><title>Disclaimer</title>

      <p id="d1e4700">Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.</p>
  </notes><notes notes-type="financialsupport"><title>Financial support</title>

      <p id="d1e4706">This research has been supported by the National Natural Science Foundation of China (grant no. 41907396), the Science and Technology
Research Program of the Chongqing Municipal Education Commission (grant no. KJQN201900535), the Chongqing Normal University Funding Program (grant no. 21XWB007), the Chongqing Normal University Postgraduate Research and
Innovation Project (grant no. YKC21047), and the Scientific Research Project
of the Department of Natural Resources of the Province of Sichuan (grant no. KJ-2021-14).</p>
  </notes><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d1e4712">This paper was edited by David J. Peres and reviewed by Hernans Martinez and one anonymous referee.</p>
  </notes><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><?label 1?><mixed-citation>Booker, A. J., Dennis, J. E., Rank, P. D., Serafini, D. B., Torczon, V., and Trosset, M. W. A rigorous framework for optimization of expensive functions by surrogates, Struct. Optimization, 17, 1–13,
<ext-link xlink:href="https://doi.org/10.1007/BF01197708" ext-link-type="DOI">10.1007/BF01197708</ext-link>, 1999.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><?label 1?><mixed-citation>Chen, M., Tang, C., Zhang, X., Xiong, J., and Li, M.: Quantitative
assessment of physical fragility of buildings to the debris flow on 20 August 2019 in the Cutou gully, Wenchuan, southwestern China, Eng. Geol., 293, 106319, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2021.106319" ext-link-type="DOI">10.1016/j.enggeo.2021.106319</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><?label 1?><mixed-citation>Choi, S. K., Lee, J. M., and Kwon, T. H.: Effect of slit-type barrier on
characteristics of water-dominant debris flows: small-scale physical
modeling, Landslides, 15, 111–122, <ext-link xlink:href="https://doi.org/10.1007/s10346-017-0853-4" ext-link-type="DOI">10.1007/s10346-017-0853-4</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><?label 1?><mixed-citation>Dall'Osso, F., Gonella, M., Gabbianelli, G., Withycombe, G., and Dominey-Howes, D.: A revised (PTVA) model for assessing the vulnerability of buildings to tsunami damage, Nat. Hazards Earth Syst. Sci., 9, 1557–1565, <ext-link xlink:href="https://doi.org/10.5194/nhess-9-1557-2009" ext-link-type="DOI">10.5194/nhess-9-1557-2009</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><?label 1?><mixed-citation>Dall'Osso, F., Dominey-Howes, D., Tarbotton, C., Summerhayes, S., and
Withycombe, G.: Revision and improvement of the PTVA-3 model for assessing
tsunami building vulnerability using “international expert judgment”:
introducing the PTVA-4 model, Nat. Hazards, 83, 1229–1256,
<ext-link xlink:href="https://doi.org/10.1007/s11069-016-2387-9" ext-link-type="DOI">10.1007/s11069-016-2387-9</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><?label 1?><mixed-citation>Faisal, N. A. A., Ghani, A., and Salim, N.: The ability of wall openings to
reduce flood induced forces on residential building, International Journal
of GEOMATE, 14, 63–69, <ext-link xlink:href="https://doi.org/10.21660/2018.46.7306" ext-link-type="DOI">10.21660/2018.46.7306</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><?label 1?><mixed-citation>
Flow Science, Inc.: FLOW-3D v11.0.3 User Manual, Santa Fe, USA, 2014.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><?label 1?><mixed-citation>Franco, A., Moernaut, J., Schneider-Muntau, B., Strasser, M., and Gems, B.:
Triggers and consequences of landslide-induced impulse waves-3D dynamic
reconstruction of the Taan Fiord 2015 tsunami event, Eng. Geol.,
294, 106384, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2021.106384" ext-link-type="DOI">10.1016/j.enggeo.2021.106384</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><?label 1?><mixed-citation>Fuchs, S., Ornetsmüller, C., and Totschnig, R.: Spatial scan statistics in vulnerability assessment: an application to mountain hazards, Nat. Hazards, 64, 2129–2151, <ext-link xlink:href="https://doi.org/10.1007/s11069-011-0081-5" ext-link-type="DOI">10.1007/s11069-011-0081-5</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><?label 1?><mixed-citation>Fuchs, S., Keiler, M., and Zischg, A.: A spatiotemporal multi-hazard exposure assessment based on property data, Nat. Hazards Earth Syst. Sci., 15, 2127–2142, <ext-link xlink:href="https://doi.org/10.5194/nhess-15-2127-2015" ext-link-type="DOI">10.5194/nhess-15-2127-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><?label 1?><mixed-citation>Fuchs, S., Röthlisberger, V., Thaler, T., Zischg, A., and Keiler, M.:
Natural hazard management from a coevolutionary perspective: Exposure and
policy response in the European Alps, Ann. Am. Assoc. Geogr., 107, 382–392, <ext-link xlink:href="https://doi.org/10.1080/24694452.2016.1235494" ext-link-type="DOI">10.1080/24694452.2016.1235494</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><?label 1?><mixed-citation>Fuchs, S., Keiler, M., Ortlepp, R., Schinke, R., and Papathoma-Köhle,
M.: Recent advances in vulnerability assessment for the built environment
exposed to torrential hazards: Challenges and the way forward, J.
Hydrol., 575, 587–595, <ext-link xlink:href="https://doi.org/10.1016/j.jhydrol.2019.05.067" ext-link-type="DOI">10.1016/j.jhydrol.2019.05.067</ext-link>, 2019.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><?label 1?><mixed-citation>Gao, L., Zhang, L. M., and Chen, H. X.: Two-dimensional simulation of debris
flow impact pressures on buildings, Eng. Geol., 226, 236–244,
<ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2017.06.012" ext-link-type="DOI">10.1016/j.enggeo.2017.06.012</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><?label 1?><mixed-citation>Gems, B., Mazzorana, B., Hofer, T., Sturm, M., Gabl, R., and Aufleger, M.: 3-D hydrodynamic modelling of flood impacts on a building and indoor flooding processes, Nat. Hazards Earth Syst. Sci., 16, 1351–1368, <ext-link xlink:href="https://doi.org/10.5194/nhess-16-1351-2016" ext-link-type="DOI">10.5194/nhess-16-1351-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><?label 1?><mixed-citation>Gomez-Gesteira, M. and Dalrymple, R. A.: Using a three-dimensional smoothed
particle hydrodynamics method for wave impact on a tall structure, J. Waterw.
Port. Coast., 130, 63–69, <ext-link xlink:href="https://doi.org/10.1061/(ASCE)0733-950X(2004)130:2(63)" ext-link-type="DOI">10.1061/(ASCE)0733-950X(2004)130:2(63)</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><?label 1?><mixed-citation>Hirt, C. W. and Nichols, B. D.: Volume of fluid (VOF) method for the dynamics
of free boundaries, J. Comput. Phys., 39, 201–225,
<ext-link xlink:href="https://doi.org/10.1016/0021-9991(81)90145-5" ext-link-type="DOI">10.1016/0021-9991(81)90145-5</ext-link>, 1981.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><?label 1?><mixed-citation>Hirt, C. W. and Sicilian, J. M.: A porosity technique for the definition of
obstacles in rectangular cell meshes, 4th International Conference on
Numerical Ship Hydrodynamics, Washington, D.C., 24 September 1985, 1–19, <uri>https://trid.trb.org/view/394627</uri> (last access: 23 February 2023), 1985.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><?label 1?><mixed-citation>Hoffman, R. M., Sudjianto, A., Du, X., and Stout, J.: Robust piston design
and optimization using piston secondary motion analysis, SAE Technical Paper, No. 2003-01-0148, <ext-link xlink:href="https://doi.org/10.4271/2003-01-0148" ext-link-type="DOI">10.4271/2003-01-0148</ext-link>, 2003.</mixed-citation></ref>
      <ref id="bib1.bib19"><label>19</label><?label 1?><mixed-citation>Holub, M. and Fuchs, S.: Mitigating mountain hazards in Austria – legislation, risk transfer, and awareness building, Nat. Hazards Earth Syst. Sci., 9, 523–537, <ext-link xlink:href="https://doi.org/10.5194/nhess-9-523-2009" ext-link-type="DOI">10.5194/nhess-9-523-2009</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib20"><label>20</label><?label 1?><mixed-citation>Holub, M., Suda, J., and Fuchs, S.: Mountain hazards: reducing vulnerability
by adapted building design, Environ. Earth Sci., 66, 1853–1870,
<ext-link xlink:href="https://doi.org/10.1007/s12665-011-1410-4" ext-link-type="DOI">10.1007/s12665-011-1410-4</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib21"><label>21</label><?label 1?><mixed-citation>Hu, K. H., Cui, P., and Zhang, J. Q.: Characteristics of damage to buildings by debris flows on 7 August 2010 in Zhouqu, Western China, Nat. Hazards Earth Syst. Sci., 12, 2209–2217, <ext-link xlink:href="https://doi.org/10.5194/nhess-12-2209-2012" ext-link-type="DOI">10.5194/nhess-12-2209-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib22"><label>22</label><?label 1?><mixed-citation>Hu, Y., Chen, M., and Zhou, J.: Numerical simulation of the entrainment
effect during mass movement in high-speed debris avalanches, Arab. J. Geosci., 12, 14, <ext-link xlink:href="https://doi.org/10.1007/s12517-018-4199-6" ext-link-type="DOI">10.1007/s12517-018-4199-6</ext-link>, 2019.</mixed-citation></ref>
      <ref id="bib1.bib23"><label>23</label><?label 1?><mixed-citation>Hu, Y., Yu, Z., and Zhou, J.: Numerical simulation of landslide-generated
waves during the 11 October 2018 Baige landslide at the Jinsha River,
Landslides, 17, 2317–2328, <ext-link xlink:href="https://doi.org/10.1007/s10346-020-01382-x" ext-link-type="DOI">10.1007/s10346-020-01382-x</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib24"><label>24</label><?label 1?><mixed-citation>Huang, X. and Tang, C.: Formation and activation of catastrophic debris
flows in Baishui River basin, Sichuan Province, China, Landslides, 11,
955–967, <ext-link xlink:href="https://doi.org/10.1007/s10346-014-0465-1" ext-link-type="DOI">10.1007/s10346-014-0465-1</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib25"><label>25</label><?label 1?><mixed-citation>Iverson, R. M., Logan, M., Lahusen, R. G., and Berti, M.: The perfect debris
flow? Aggregated results from 28 large-scale experiments, J. Geophys. Res.-Earth, 115, F03005, <ext-link xlink:href="https://doi.org/10.1029/2009JF001514" ext-link-type="DOI">10.1029/2009JF001514</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib26"><label>26</label><?label 1?><mixed-citation>Jakob, M., Stein, D., and Ulmi M.: Vulnerability of buildings to debris flow
impact, Nat. Hazards, 60, 241–261, <ext-link xlink:href="https://doi.org/10.1007/s11069-011-0007-2" ext-link-type="DOI">10.1007/s11069-011-0007-2</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib27"><label>27</label><?label 1?><mixed-citation>Jones, W. P. and Launder, B. E.: The prediction of laminarization with a
two-equation model of turbulence, Int. J. Heat Mass Tran., 15, 301–314,
<ext-link xlink:href="https://doi.org/10.1016/0017-9310(72)90076-2" ext-link-type="DOI">10.1016/0017-9310(72)90076-2</ext-link>​​​​​​​, 1972.</mixed-citation></ref>
      <ref id="bib1.bib28"><label>28</label><?label 1?><mixed-citation>Kim, M., Lee, S., Kwon, T., Choi, S., and Jeon, J.: Sensitivity analysis of
influencing parameters on slit-type barrier performance against debris flow
using 3D-based numerical approach, Intt. J. Sediment Res., 36, 50–62, <ext-link xlink:href="https://doi.org/10.1016/j.ijsrc.2020.04.005" ext-link-type="DOI">10.1016/j.ijsrc.2020.04.005</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib29"><label>29</label><?label 1?><mixed-citation>Kim, M. J., Lee, S. R., Jeon, J. S., and Yoon, S.: Sensitivity analysis of
bentonite buffer peak temperature in a high-level waste repository, Ann. Nucl. Energy, 123, 190–199, <ext-link xlink:href="https://doi.org/10.1016/j.anucene.2018.09.020" ext-link-type="DOI">10.1016/j.anucene.2018.09.020</ext-link>, 2019.</mixed-citation></ref>
      <ref id="bib1.bib30"><label>30</label><?label 1?><mixed-citation>Kleijnen, J. P. C.: Regression and Kriging metamodels with their
experimental designs in simulation: A review, Eur. J. Oper. Res., 256, 1–16,
<ext-link xlink:href="https://doi.org/10.1016/j.ejor.2016.06.041" ext-link-type="DOI">10.1016/j.ejor.2016.06.041</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib31"><label>31</label><?label 1?><mixed-citation>Kucherenko, S. and Zaccheus, O.​​​​​​​: SobolGSA mode, Imperial College London [code], <uri>https://www.imperial.ac.uk/process-systems-engineering/research/free-software/sobolgsa-software/</uri>, last access: 23 February 2023.</mixed-citation></ref>
      <ref id="bib1.bib32"><label>32</label><?label 1?><mixed-citation>Kucherenko, S., Albrecht, D., and Saltelli, A.: Exploring multi-dimensional
spaces: a Comparison of Latin Hypercube and Quasi Monte Carlo Sampling
Techniques, arXiv [preprint], <ext-link xlink:href="https://doi.org/10.48550/arXiv.1505.02350" ext-link-type="DOI">10.48550/arXiv.1505.02350</ext-link>, 10 May 2015.</mixed-citation></ref>
      <?pagebreak page889?><ref id="bib1.bib33"><label>33</label><?label 1?><mixed-citation>Liang, H., Li, J., Liu, F., Zhang, L., Gang, F., Li, M., and He, S.:
Simulation of debris flow impacting bridge pier tests based on smooth
particle hydromechanics method, Rock and Soil Mechanics, 42, 1473–1484,
<ext-link xlink:href="https://doi.org/10.16285/j.rsm.2020.1107" ext-link-type="DOI">10.16285/j.rsm.2020.1107</ext-link>, 2021 (in Chinese with English
abstract).</mixed-citation></ref>
      <ref id="bib1.bib34"><label>34</label><?label 1?><mixed-citation>Liu, C., Yu, Z., and Zhao, S.: A coupled SPH-DEM-FEM model for
fluid-particle-structure interaction and a case study of Wenjia gully debris
flow impact estimation, Landslides, 18, 2403–2425,
<ext-link xlink:href="https://doi.org/10.1007/s10346-021-01640-6" ext-link-type="DOI">10.1007/s10346-021-01640-6</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib35"><label>35</label><?label 1?><mixed-citation>Luo, H. Y., Fan, R. L., Wang, H. J., and Zhang, L. M.: Physics of building
vulnerability to debris flows, floods and earth flows, Eng. Geol., 271, 105611, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2020.105611" ext-link-type="DOI">10.1016/j.enggeo.2020.105611</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib36"><label>36</label><?label 1?><mixed-citation>Manawasekara, C., Mizutani, N., and Aoki, S.: Influence of openings and
orientation on tsunami generated forces on buildings, Journal of Disaster
Research, 11, 670–679, <ext-link xlink:href="https://doi.org/10.20965/jdr.2016.p0670" ext-link-type="DOI">10.20965/jdr.2016.p0670</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib37"><label>37</label><?label 1?><mixed-citation>Martinez-Carvajal, H. E., de Moraes Guimaraes Silva, M. T.,
Garcia-Aristizabal, E. F., Aristizabal-Giraldo, E. V., and Larios-Benavides, M. A.: A mathematical approach for assessing landslide vulnerability, Earth
Sci. Res. J., 22, 251–273, <ext-link xlink:href="https://doi.org/10.15446/esrj.v22n4.68553" ext-link-type="DOI">10.15446/esrj.v22n4.68553</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib38"><label>38</label><?label 1?><mixed-citation>Mazzorana, B., Simoni, S., Scherer, C., Gems, B., Fuchs, S., and Keiler, M.: A physical approach on flood risk vulnerability of buildings, Hydrol. Earth Syst. Sci., 18, 3817–3836, <ext-link xlink:href="https://doi.org/10.5194/hess-18-3817-2014" ext-link-type="DOI">10.5194/hess-18-3817-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib39"><label>39</label><?label 1?><mixed-citation>Mead, S. R., Magill, C., Lemiale, V., Thouret, J.-C., and Prakash, M.: Examining the impact of lahars on buildings using numerical modelling, Nat. Hazards Earth Syst. Sci., 17, 703–719, <ext-link xlink:href="https://doi.org/10.5194/nhess-17-703-2017" ext-link-type="DOI">10.5194/nhess-17-703-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib40"><label>40</label><?label 1?><mixed-citation>Papathoma-Köhle, M.: Vulnerability curves vs. vulnerability indicators: application of an indicator-based methodology for debris-flow hazards, Nat. Hazards Earth Syst. Sci., 16, 1771–1790, <ext-link xlink:href="https://doi.org/10.5194/nhess-16-1771-2016" ext-link-type="DOI">10.5194/nhess-16-1771-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib41"><label>41</label><?label 1?><mixed-citation>Papathoma-Köhle, M., Gems, B., Sturm, M., and Fuchs, S.: Matrices,
curves and indicators: A review of approaches to assess physical
vulnerability to debris flows, Earth-Sci. Rev., 171, 272–288,
<ext-link xlink:href="https://doi.org/10.1016/j.earscirev.2017.06.007" ext-link-type="DOI">10.1016/j.earscirev.2017.06.007</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib42"><label>42</label><?label 1?><mixed-citation>Papathoma-Köhle, M., Schlögl, M., and Fuchs, S.: Vulnerability
indicators for natural hazards: an innovative selection and weighting
approach, Sci. Rep., 9, 15026, <ext-link xlink:href="https://doi.org/10.1038/s41598-019-50257-2" ext-link-type="DOI">10.1038/s41598-019-50257-2</ext-link>, 2019.</mixed-citation></ref>
      <ref id="bib1.bib43"><label>43</label><?label 1?><mixed-citation>Saltelli, A., Annoni, P., Azzini, I., Campolongo, F., and Tarantola, S.:
Variance based sensitivity analysis of model output. Design and estimator
for the total sensitivity index, Comput. Phys. Commun., 181,
259–270, <ext-link xlink:href="https://doi.org/10.1016/j.cpc.2009.09.018" ext-link-type="DOI">10.1016/j.cpc.2009.09.018</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib44"><label>44</label><?label 1?><mixed-citation>Sarrazin, F., Pianosi, F., and Wagener, T.: Global sensitivity analysis of
environmental models: Convergence and validation, Environ. Modell. Softw., 79, 135–152, <ext-link xlink:href="https://doi.org/10.1016/j.envsoft.2016.02.005" ext-link-type="DOI">10.1016/j.envsoft.2016.02.005</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib45"><label>45</label><?label 1?><mixed-citation>
Sobol, I. M.: Sensitivity estimates for nonlinear mathematical models,
Math. Model. Comput. Exp,, 1, 407–414, 1993.</mixed-citation></ref>
      <ref id="bib1.bib46"><label>46</label><?label 1?><mixed-citation>Sobol, I. M., Asotsky, D., Kreinin, A., and Kucherenko, S.: Construction and
comparison of high-dimensional Sobol' generators, Wilmott, 2011, 64–79,
<ext-link xlink:href="https://doi.org/10.1002/wilm.10056" ext-link-type="DOI">10.1002/wilm.10056</ext-link>, 2011.
</mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib47"><label>47</label><?label 1?><mixed-citation>Song, D., Chen, X., Zhou, G. G. D., Lu, X., Cheng, G., and Chen, Q.: Impact
dynamics of debris flow against rigid obstacle in laboratory experiments,
Eng. Geol., 291, 106211, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2021.106211" ext-link-type="DOI">10.1016/j.enggeo.2021.106211</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib48"><label>48</label><?label 1?><mixed-citation>Sturm, M., Gems, B., Keller, F., Mazzorana, B., Fuchs, S.,
Papathoma-Köhle, M., and Aufleger, M.: Understanding impact dynamics on
buildings caused by fluviatile sediment transport, Geomorphology, 321,
45–59, <ext-link xlink:href="https://doi.org/10.1016/j.geomorph.2018.08.016" ext-link-type="DOI">10.1016/j.geomorph.2018.08.016</ext-link>, 2018a.</mixed-citation></ref>
      <ref id="bib1.bib49"><label>49</label><?label 1?><mixed-citation>Sturm, M., Gems, B., Keller, F., Mazzorana, B., Fuchs, S.,
Papathoma-Köhle, M., and Aufleger, M.: Experimental analyses of impact
forces on buildings exposed to fluvial hazards, J. Hydrol., 565,
1–13, <ext-link xlink:href="https://doi.org/10.1016/j.jhydrol.2018.07.070" ext-link-type="DOI">10.1016/j.jhydrol.2018.07.070</ext-link>, 2018b.</mixed-citation></ref>
      <ref id="bib1.bib50"><label>50</label><?label 1?><mixed-citation>
Takahashi, T.: Debris Flow Mechanics, Prediction and Countermeasures, Taylor
&amp; Francis Group, London, UK, ISBN 978-0-203-94628-2, 2007.</mixed-citation></ref>
      <ref id="bib1.bib51"><label>51</label><?label 1?><mixed-citation>Tang, C., Rengers, N., van Asch, Th. W. J., Yang, Y. H., and Wang, G. F.: Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China, Nat. Hazards Earth Syst. Sci., 11, 2903–2912, <ext-link xlink:href="https://doi.org/10.5194/nhess-11-2903-2011" ext-link-type="DOI">10.5194/nhess-11-2903-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib52"><label>52</label><?label 1?><mixed-citation>Totschnig, R., Sedlacek, W., and Fuchs, S.: A quantitative vulnerability
function for fluvial sediment transport, Nat. Hazards, 58, 681–703,
<ext-link xlink:href="https://doi.org/10.1007/s11069-010-9623-5" ext-link-type="DOI">10.1007/s11069-010-9623-5</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib53"><label>53</label><?label 1?><mixed-citation>Yin, Y. P., Huang, B., Chen, X., Liu, G., and Wang, S.: Numerical analysis
on wave generated by the Qianjiangping landslide in Three Gorges Reservoir,
China, Landslides, 12, 355–364, <ext-link xlink:href="https://doi.org/10.1007/s10346-015-0564-7" ext-link-type="DOI">10.1007/s10346-015-0564-7</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib54"><label>54</label><?label 1?><mixed-citation>Zeng, C., Cui, P., Su, Z., Lei, Y., and Chen, R.: Failure modes of
reinforced concrete columns of buildings under debris flow impact,
Landslides, 12, 561–571, <ext-link xlink:href="https://doi.org/10.1007/s10346-014-0490-0" ext-link-type="DOI">10.1007/s10346-014-0490-0</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib55"><label>55</label><?label 1?><mixed-citation>Zhang, J., Termaath, S., and Shields M. D.: Imprecise global sensitivity
analysis using bayesian multimodel inference and importance sampling,
Mech. Syst. Signal Pr., 148, 107162, <ext-link xlink:href="https://doi.org/10.1016/j.ymssp.2020.107162" ext-link-type="DOI">10.1016/j.ymssp.2020.107162</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib56"><label>56</label><?label 1?><mixed-citation>Zhang, S., Zhang, L., Li, X., and Xu, Q.: Physical vulnerability models for
assessing building damage by debris flows, Eng. Geol., 247,
145–158, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2018.10.017" ext-link-type="DOI">10.1016/j.enggeo.2018.10.017</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib57"><label>57</label><?label 1?><mixed-citation>Zhang, Y., Chen, J., Tan, C., Bao, Y., Han, X., Yan, J., and Mehmood, Q.: A
novel approach to simulating debris flow runout via a three-dimensional CFD
code: a case study of Xiaojia Gully, B. Eng. Geol. Environ., 80, 5293–5313, <ext-link xlink:href="https://doi.org/10.1007/s10064-021-02270-x" ext-link-type="DOI">10.1007/s10064-021-02270-x</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib58"><label>58</label><?label 1?><mixed-citation>Zhuang, Y., Yin, Y., Xing, A., and Jin, K.: Combined numerical investigation
of the Yigong rock slide-debris avalanche and subsequent dam-break flood
propagation in Tibet, China, Landslides, 17, 2217–2229,
<ext-link xlink:href="https://doi.org/10.1007/s10346-020-01449-9" ext-link-type="DOI">10.1007/s10346-020-01449-9</ext-link>, 2020.</mixed-citation></ref>

  </ref-list></back>
    <!--<article-title-html>Sensitivity analysis of a built environment exposed to the synthetic monophasic viscous debris flow impacts with 3-D numerical simulations</article-title-html>
<abstract-html/>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
      
Booker, A. J., Dennis, J. E., Rank, P. D., Serafini, D. B., Torczon, V., and Trosset, M. W. A rigorous framework for optimization of expensive functions by surrogates, Struct. Optimization, 17, 1–13,
<a href="https://doi.org/10.1007/BF01197708" target="_blank">https://doi.org/10.1007/BF01197708</a>, 1999.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
      
Chen, M., Tang, C., Zhang, X., Xiong, J., and Li, M.: Quantitative
assessment of physical fragility of buildings to the debris flow on 20 August 2019 in the Cutou gully, Wenchuan, southwestern China, Eng. Geol., 293, 106319, <a href="https://doi.org/10.1016/j.enggeo.2021.106319" target="_blank">https://doi.org/10.1016/j.enggeo.2021.106319</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
      
Choi, S. K., Lee, J. M., and Kwon, T. H.: Effect of slit-type barrier on
characteristics of water-dominant debris flows: small-scale physical
modeling, Landslides, 15, 111–122, <a href="https://doi.org/10.1007/s10346-017-0853-4" target="_blank">https://doi.org/10.1007/s10346-017-0853-4</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
      
Dall'Osso, F., Gonella, M., Gabbianelli, G., Withycombe, G., and Dominey-Howes, D.: A revised (PTVA) model for assessing the vulnerability of buildings to tsunami damage, Nat. Hazards Earth Syst. Sci., 9, 1557–1565, <a href="https://doi.org/10.5194/nhess-9-1557-2009" target="_blank">https://doi.org/10.5194/nhess-9-1557-2009</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
      
Dall'Osso, F., Dominey-Howes, D., Tarbotton, C., Summerhayes, S., and
Withycombe, G.: Revision and improvement of the PTVA-3 model for assessing
tsunami building vulnerability using “international expert judgment”:
introducing the PTVA-4 model, Nat. Hazards, 83, 1229–1256,
<a href="https://doi.org/10.1007/s11069-016-2387-9" target="_blank">https://doi.org/10.1007/s11069-016-2387-9</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
      
Faisal, N. A. A., Ghani, A., and Salim, N.: The ability of wall openings to
reduce flood induced forces on residential building, International Journal
of GEOMATE, 14, 63–69, <a href="https://doi.org/10.21660/2018.46.7306" target="_blank">https://doi.org/10.21660/2018.46.7306</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
      
Flow Science, Inc.: FLOW-3D v11.0.3 User Manual, Santa Fe, USA, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
      
Franco, A., Moernaut, J., Schneider-Muntau, B., Strasser, M., and Gems, B.:
Triggers and consequences of landslide-induced impulse waves-3D dynamic
reconstruction of the Taan Fiord 2015 tsunami event, Eng. Geol.,
294, 106384, <a href="https://doi.org/10.1016/j.enggeo.2021.106384" target="_blank">https://doi.org/10.1016/j.enggeo.2021.106384</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation>
      
Fuchs, S., Ornetsmüller, C., and Totschnig, R.: Spatial scan statistics in vulnerability assessment: an application to mountain hazards, Nat. Hazards, 64, 2129–2151, <a href="https://doi.org/10.1007/s11069-011-0081-5" target="_blank">https://doi.org/10.1007/s11069-011-0081-5</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
      
Fuchs, S., Keiler, M., and Zischg, A.: A spatiotemporal multi-hazard exposure assessment based on property data, Nat. Hazards Earth Syst. Sci., 15, 2127–2142, <a href="https://doi.org/10.5194/nhess-15-2127-2015" target="_blank">https://doi.org/10.5194/nhess-15-2127-2015</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
      
Fuchs, S., Röthlisberger, V., Thaler, T., Zischg, A., and Keiler, M.:
Natural hazard management from a coevolutionary perspective: Exposure and
policy response in the European Alps, Ann. Am. Assoc. Geogr., 107, 382–392, <a href="https://doi.org/10.1080/24694452.2016.1235494" target="_blank">https://doi.org/10.1080/24694452.2016.1235494</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
      
Fuchs, S., Keiler, M., Ortlepp, R., Schinke, R., and Papathoma-Köhle,
M.: Recent advances in vulnerability assessment for the built environment
exposed to torrential hazards: Challenges and the way forward, J.
Hydrol., 575, 587–595, <a href="https://doi.org/10.1016/j.jhydrol.2019.05.067" target="_blank">https://doi.org/10.1016/j.jhydrol.2019.05.067</a>, 2019.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
      
Gao, L., Zhang, L. M., and Chen, H. X.: Two-dimensional simulation of debris
flow impact pressures on buildings, Eng. Geol., 226, 236–244,
<a href="https://doi.org/10.1016/j.enggeo.2017.06.012" target="_blank">https://doi.org/10.1016/j.enggeo.2017.06.012</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
      
Gems, B., Mazzorana, B., Hofer, T., Sturm, M., Gabl, R., and Aufleger, M.: 3-D hydrodynamic modelling of flood impacts on a building and indoor flooding processes, Nat. Hazards Earth Syst. Sci., 16, 1351–1368, <a href="https://doi.org/10.5194/nhess-16-1351-2016" target="_blank">https://doi.org/10.5194/nhess-16-1351-2016</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation>
      
Gomez-Gesteira, M. and Dalrymple, R. A.: Using a three-dimensional smoothed
particle hydrodynamics method for wave impact on a tall structure, J. Waterw.
Port. Coast., 130, 63–69, <a href="https://doi.org/10.1061/(ASCE)0733-950X(2004)130:2(63)" target="_blank">https://doi.org/10.1061/(ASCE)0733-950X(2004)130:2(63)</a>, 2004.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation>
      
Hirt, C. W. and Nichols, B. D.: Volume of fluid (VOF) method for the dynamics
of free boundaries, J. Comput. Phys., 39, 201–225,
<a href="https://doi.org/10.1016/0021-9991(81)90145-5" target="_blank">https://doi.org/10.1016/0021-9991(81)90145-5</a>, 1981.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation>
      
Hirt, C. W. and Sicilian, J. M.: A porosity technique for the definition of
obstacles in rectangular cell meshes, 4th International Conference on
Numerical Ship Hydrodynamics, Washington, D.C., 24 September 1985, 1–19, <a href="https://trid.trb.org/view/394627" target="_blank"/> (last access: 23 February 2023), 1985.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
      
Hoffman, R. M., Sudjianto, A., Du, X., and Stout, J.: Robust piston design
and optimization using piston secondary motion analysis, SAE Technical Paper, No. 2003-01-0148, <a href="https://doi.org/10.4271/2003-01-0148" target="_blank">https://doi.org/10.4271/2003-01-0148</a>, 2003.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
      
Holub, M. and Fuchs, S.: Mitigating mountain hazards in Austria – legislation, risk transfer, and awareness building, Nat. Hazards Earth Syst. Sci., 9, 523–537, <a href="https://doi.org/10.5194/nhess-9-523-2009" target="_blank">https://doi.org/10.5194/nhess-9-523-2009</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation>
      
Holub, M., Suda, J., and Fuchs, S.: Mountain hazards: reducing vulnerability
by adapted building design, Environ. Earth Sci., 66, 1853–1870,
<a href="https://doi.org/10.1007/s12665-011-1410-4" target="_blank">https://doi.org/10.1007/s12665-011-1410-4</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib21"><label>21</label><mixed-citation>
      
Hu, K. H., Cui, P., and Zhang, J. Q.: Characteristics of damage to buildings by debris flows on 7 August 2010 in Zhouqu, Western China, Nat. Hazards Earth Syst. Sci., 12, 2209–2217, <a href="https://doi.org/10.5194/nhess-12-2209-2012" target="_blank">https://doi.org/10.5194/nhess-12-2209-2012</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib22"><label>22</label><mixed-citation>
      
Hu, Y., Chen, M., and Zhou, J.: Numerical simulation of the entrainment
effect during mass movement in high-speed debris avalanches, Arab. J. Geosci., 12, 14, <a href="https://doi.org/10.1007/s12517-018-4199-6" target="_blank">https://doi.org/10.1007/s12517-018-4199-6</a>, 2019.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib23"><label>23</label><mixed-citation>
      
Hu, Y., Yu, Z., and Zhou, J.: Numerical simulation of landslide-generated
waves during the 11 October 2018 Baige landslide at the Jinsha River,
Landslides, 17, 2317–2328, <a href="https://doi.org/10.1007/s10346-020-01382-x" target="_blank">https://doi.org/10.1007/s10346-020-01382-x</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib24"><label>24</label><mixed-citation>
      
Huang, X. and Tang, C.: Formation and activation of catastrophic debris
flows in Baishui River basin, Sichuan Province, China, Landslides, 11,
955–967, <a href="https://doi.org/10.1007/s10346-014-0465-1" target="_blank">https://doi.org/10.1007/s10346-014-0465-1</a>, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib25"><label>25</label><mixed-citation>
      
Iverson, R. M., Logan, M., Lahusen, R. G., and Berti, M.: The perfect debris
flow? Aggregated results from 28 large-scale experiments, J. Geophys. Res.-Earth, 115, F03005, <a href="https://doi.org/10.1029/2009JF001514" target="_blank">https://doi.org/10.1029/2009JF001514</a>, 2010.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib26"><label>26</label><mixed-citation>
      
Jakob, M., Stein, D., and Ulmi M.: Vulnerability of buildings to debris flow
impact, Nat. Hazards, 60, 241–261, <a href="https://doi.org/10.1007/s11069-011-0007-2" target="_blank">https://doi.org/10.1007/s11069-011-0007-2</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>27</label><mixed-citation>
      
Jones, W. P. and Launder, B. E.: The prediction of laminarization with a
two-equation model of turbulence, Int. J. Heat Mass Tran., 15, 301–314,
<a href="https://doi.org/10.1016/0017-9310(72)90076-2" target="_blank">https://doi.org/10.1016/0017-9310(72)90076-2</a>​​​​​​​, 1972.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>28</label><mixed-citation>
      
Kim, M., Lee, S., Kwon, T., Choi, S., and Jeon, J.: Sensitivity analysis of
influencing parameters on slit-type barrier performance against debris flow
using 3D-based numerical approach, Intt. J. Sediment Res., 36, 50–62, <a href="https://doi.org/10.1016/j.ijsrc.2020.04.005" target="_blank">https://doi.org/10.1016/j.ijsrc.2020.04.005</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib29"><label>29</label><mixed-citation>
      
Kim, M. J., Lee, S. R., Jeon, J. S., and Yoon, S.: Sensitivity analysis of
bentonite buffer peak temperature in a high-level waste repository, Ann. Nucl. Energy, 123, 190–199, <a href="https://doi.org/10.1016/j.anucene.2018.09.020" target="_blank">https://doi.org/10.1016/j.anucene.2018.09.020</a>, 2019.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation>
      
Kleijnen, J. P. C.: Regression and Kriging metamodels with their
experimental designs in simulation: A review, Eur. J. Oper. Res., 256, 1–16,
<a href="https://doi.org/10.1016/j.ejor.2016.06.041" target="_blank">https://doi.org/10.1016/j.ejor.2016.06.041</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation>
      
Kucherenko, S. and Zaccheus, O.​​​​​​​: SobolGSA mode, Imperial College London [code], <a href="https://www.imperial.ac.uk/process-systems-engineering/research/free-software/sobolgsa-software/" target="_blank"/>, last access: 23 February 2023.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib32"><label>32</label><mixed-citation>
      
Kucherenko, S., Albrecht, D., and Saltelli, A.: Exploring multi-dimensional
spaces: a Comparison of Latin Hypercube and Quasi Monte Carlo Sampling
Techniques, arXiv [preprint], <a href="https://doi.org/10.48550/arXiv.1505.02350" target="_blank">https://doi.org/10.48550/arXiv.1505.02350</a>, 10 May 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib33"><label>33</label><mixed-citation>
      
Liang, H., Li, J., Liu, F., Zhang, L., Gang, F., Li, M., and He, S.:
Simulation of debris flow impacting bridge pier tests based on smooth
particle hydromechanics method, Rock and Soil Mechanics, 42, 1473–1484,
<a href="https://doi.org/10.16285/j.rsm.2020.1107" target="_blank">https://doi.org/10.16285/j.rsm.2020.1107</a>, 2021 (in Chinese with English
abstract).

    </mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation>
      
Liu, C., Yu, Z., and Zhao, S.: A coupled SPH-DEM-FEM model for
fluid-particle-structure interaction and a case study of Wenjia gully debris
flow impact estimation, Landslides, 18, 2403–2425,
<a href="https://doi.org/10.1007/s10346-021-01640-6" target="_blank">https://doi.org/10.1007/s10346-021-01640-6</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation>
      
Luo, H. Y., Fan, R. L., Wang, H. J., and Zhang, L. M.: Physics of building
vulnerability to debris flows, floods and earth flows, Eng. Geol., 271, 105611, <a href="https://doi.org/10.1016/j.enggeo.2020.105611" target="_blank">https://doi.org/10.1016/j.enggeo.2020.105611</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib36"><label>36</label><mixed-citation>
      
Manawasekara, C., Mizutani, N., and Aoki, S.: Influence of openings and
orientation on tsunami generated forces on buildings, Journal of Disaster
Research, 11, 670–679, <a href="https://doi.org/10.20965/jdr.2016.p0670" target="_blank">https://doi.org/10.20965/jdr.2016.p0670</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib37"><label>37</label><mixed-citation>
      
Martinez-Carvajal, H. E., de Moraes Guimaraes Silva, M. T.,
Garcia-Aristizabal, E. F., Aristizabal-Giraldo, E. V., and Larios-Benavides, M. A.: A mathematical approach for assessing landslide vulnerability, Earth
Sci. Res. J., 22, 251–273, <a href="https://doi.org/10.15446/esrj.v22n4.68553" target="_blank">https://doi.org/10.15446/esrj.v22n4.68553</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib38"><label>38</label><mixed-citation>
      
Mazzorana, B., Simoni, S., Scherer, C., Gems, B., Fuchs, S., and Keiler, M.: A physical approach on flood risk vulnerability of buildings, Hydrol. Earth Syst. Sci., 18, 3817–3836, <a href="https://doi.org/10.5194/hess-18-3817-2014" target="_blank">https://doi.org/10.5194/hess-18-3817-2014</a>, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib39"><label>39</label><mixed-citation>
      
Mead, S. R., Magill, C., Lemiale, V., Thouret, J.-C., and Prakash, M.: Examining the impact of lahars on buildings using numerical modelling, Nat. Hazards Earth Syst. Sci., 17, 703–719, <a href="https://doi.org/10.5194/nhess-17-703-2017" target="_blank">https://doi.org/10.5194/nhess-17-703-2017</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib40"><label>40</label><mixed-citation>
      
Papathoma-Köhle, M.: Vulnerability curves vs. vulnerability indicators: application of an indicator-based methodology for debris-flow hazards, Nat. Hazards Earth Syst. Sci., 16, 1771–1790, <a href="https://doi.org/10.5194/nhess-16-1771-2016" target="_blank">https://doi.org/10.5194/nhess-16-1771-2016</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib41"><label>41</label><mixed-citation>
      
Papathoma-Köhle, M., Gems, B., Sturm, M., and Fuchs, S.: Matrices,
curves and indicators: A review of approaches to assess physical
vulnerability to debris flows, Earth-Sci. Rev., 171, 272–288,
<a href="https://doi.org/10.1016/j.earscirev.2017.06.007" target="_blank">https://doi.org/10.1016/j.earscirev.2017.06.007</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib42"><label>42</label><mixed-citation>
      
Papathoma-Köhle, M., Schlögl, M., and Fuchs, S.: Vulnerability
indicators for natural hazards: an innovative selection and weighting
approach, Sci. Rep., 9, 15026, <a href="https://doi.org/10.1038/s41598-019-50257-2" target="_blank">https://doi.org/10.1038/s41598-019-50257-2</a>, 2019.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib43"><label>43</label><mixed-citation>
      
Saltelli, A., Annoni, P., Azzini, I., Campolongo, F., and Tarantola, S.:
Variance based sensitivity analysis of model output. Design and estimator
for the total sensitivity index, Comput. Phys. Commun., 181,
259–270, <a href="https://doi.org/10.1016/j.cpc.2009.09.018" target="_blank">https://doi.org/10.1016/j.cpc.2009.09.018</a>, 2010.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib44"><label>44</label><mixed-citation>
      
Sarrazin, F., Pianosi, F., and Wagener, T.: Global sensitivity analysis of
environmental models: Convergence and validation, Environ. Modell. Softw., 79, 135–152, <a href="https://doi.org/10.1016/j.envsoft.2016.02.005" target="_blank">https://doi.org/10.1016/j.envsoft.2016.02.005</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib45"><label>45</label><mixed-citation>
      
Sobol, I. M.: Sensitivity estimates for nonlinear mathematical models,
Math. Model. Comput. Exp,, 1, 407–414, 1993.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib46"><label>46</label><mixed-citation>
      
Sobol, I. M., Asotsky, D., Kreinin, A., and Kucherenko, S.: Construction and
comparison of high-dimensional Sobol' generators, Wilmott, 2011, 64–79,
<a href="https://doi.org/10.1002/wilm.10056" target="_blank">https://doi.org/10.1002/wilm.10056</a>, 2011.


    </mixed-citation></ref-html>
<ref-html id="bib1.bib47"><label>47</label><mixed-citation>
      
Song, D., Chen, X., Zhou, G. G. D., Lu, X., Cheng, G., and Chen, Q.: Impact
dynamics of debris flow against rigid obstacle in laboratory experiments,
Eng. Geol., 291, 106211, <a href="https://doi.org/10.1016/j.enggeo.2021.106211" target="_blank">https://doi.org/10.1016/j.enggeo.2021.106211</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib48"><label>48</label><mixed-citation>
      
Sturm, M., Gems, B., Keller, F., Mazzorana, B., Fuchs, S.,
Papathoma-Köhle, M., and Aufleger, M.: Understanding impact dynamics on
buildings caused by fluviatile sediment transport, Geomorphology, 321,
45–59, <a href="https://doi.org/10.1016/j.geomorph.2018.08.016" target="_blank">https://doi.org/10.1016/j.geomorph.2018.08.016</a>, 2018a.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib49"><label>49</label><mixed-citation>
      
Sturm, M., Gems, B., Keller, F., Mazzorana, B., Fuchs, S.,
Papathoma-Köhle, M., and Aufleger, M.: Experimental analyses of impact
forces on buildings exposed to fluvial hazards, J. Hydrol., 565,
1–13, <a href="https://doi.org/10.1016/j.jhydrol.2018.07.070" target="_blank">https://doi.org/10.1016/j.jhydrol.2018.07.070</a>, 2018b.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib50"><label>50</label><mixed-citation>
      
Takahashi, T.: Debris Flow Mechanics, Prediction and Countermeasures, Taylor
&amp; Francis Group, London, UK, ISBN 978-0-203-94628-2, 2007.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib51"><label>51</label><mixed-citation>
      
Tang, C., Rengers, N., van Asch, Th. W. J., Yang, Y. H., and Wang, G. F.: Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China, Nat. Hazards Earth Syst. Sci., 11, 2903–2912, <a href="https://doi.org/10.5194/nhess-11-2903-2011" target="_blank">https://doi.org/10.5194/nhess-11-2903-2011</a>, 2011.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib52"><label>52</label><mixed-citation>
      
Totschnig, R., Sedlacek, W., and Fuchs, S.: A quantitative vulnerability
function for fluvial sediment transport, Nat. Hazards, 58, 681–703,
<a href="https://doi.org/10.1007/s11069-010-9623-5" target="_blank">https://doi.org/10.1007/s11069-010-9623-5</a>, 2011.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib53"><label>53</label><mixed-citation>
      
Yin, Y. P., Huang, B., Chen, X., Liu, G., and Wang, S.: Numerical analysis
on wave generated by the Qianjiangping landslide in Three Gorges Reservoir,
China, Landslides, 12, 355–364, <a href="https://doi.org/10.1007/s10346-015-0564-7" target="_blank">https://doi.org/10.1007/s10346-015-0564-7</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib54"><label>54</label><mixed-citation>
      
Zeng, C., Cui, P., Su, Z., Lei, Y., and Chen, R.: Failure modes of
reinforced concrete columns of buildings under debris flow impact,
Landslides, 12, 561–571, <a href="https://doi.org/10.1007/s10346-014-0490-0" target="_blank">https://doi.org/10.1007/s10346-014-0490-0</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib55"><label>55</label><mixed-citation>
      
Zhang, J., Termaath, S., and Shields M. D.: Imprecise global sensitivity
analysis using bayesian multimodel inference and importance sampling,
Mech. Syst. Signal Pr., 148, 107162, <a href="https://doi.org/10.1016/j.ymssp.2020.107162" target="_blank">https://doi.org/10.1016/j.ymssp.2020.107162</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib56"><label>56</label><mixed-citation>
      
Zhang, S., Zhang, L., Li, X., and Xu, Q.: Physical vulnerability models for
assessing building damage by debris flows, Eng. Geol., 247,
145–158, <a href="https://doi.org/10.1016/j.enggeo.2018.10.017" target="_blank">https://doi.org/10.1016/j.enggeo.2018.10.017</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib57"><label>57</label><mixed-citation>
      
Zhang, Y., Chen, J., Tan, C., Bao, Y., Han, X., Yan, J., and Mehmood, Q.: A
novel approach to simulating debris flow runout via a three-dimensional CFD
code: a case study of Xiaojia Gully, B. Eng. Geol. Environ., 80, 5293–5313, <a href="https://doi.org/10.1007/s10064-021-02270-x" target="_blank">https://doi.org/10.1007/s10064-021-02270-x</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib58"><label>58</label><mixed-citation>
      
Zhuang, Y., Yin, Y., Xing, A., and Jin, K.: Combined numerical investigation
of the Yigong rock slide-debris avalanche and subsequent dam-break flood
propagation in Tibet, China, Landslides, 17, 2217–2229,
<a href="https://doi.org/10.1007/s10346-020-01449-9" target="_blank">https://doi.org/10.1007/s10346-020-01449-9</a>, 2020.

    </mixed-citation></ref-html>--></article>
