<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing with OASIS Tables v3.0 20080202//EN" "journalpub-oasis3.dtd">
<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" dtd-version="3.0"><?xmltex \makeatother\@nolinetrue\makeatletter?>
  <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-17-1713-2017</article-id><title-group><article-title>Big data managing in a landslide early warning system: experience from a ground-based interferometric radar application</article-title>
      </title-group><?xmltex \runningtitle{Big data managing in a landslide early warning system}?><?xmltex \runningauthor{E.~Intrieri et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Intrieri</surname><given-names>Emanuele</given-names></name>
          <email>emanuele.intrieri@unifi.it</email>
        <ext-link>https://orcid.org/0000-0002-9227-4409</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Bardi</surname><given-names>Federica</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Fanti</surname><given-names>Riccardo</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Gigli</surname><given-names>Giovanni</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Fidolini</surname><given-names>Francesco</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Casagli</surname><given-names>Nicola</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Costanzo</surname><given-names>Sandra</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Raffo</surname><given-names>Antonio</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Di Massa</surname><given-names>Giuseppe</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Capparelli</surname><given-names>Giovanna</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-3324-8224</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Versace</surname><given-names>Pasquale</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>Department of Earth Sciences, University of Florence, via La Pira 4, 50121, Florence, Italy</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Pizzi Terra srl, via di Ripoli 207H, 50126, Florence, Italy</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Department of Informatics, Modeling, Electronics and System Engineering,
University of Calabria, Ponte Pietro Bucci, Cube 41b, 87036, Arcavacata di Rende (CS), Italy</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Emanuele Intrieri (emanuele.intrieri@unifi.it)</corresp></author-notes><pub-date><day>6</day><month>October</month><year>2017</year></pub-date>
      
      <volume>17</volume>
      <issue>10</issue>
      <fpage>1713</fpage><lpage>1723</lpage>
      <history>
        <date date-type="received"><day>19</day><month>May</month><year>2017</year></date>
           <date date-type="rev-request"><day>31</day><month>May</month><year>2017</year></date>
           <date date-type="rev-recd"><day>25</day><month>August</month><year>2017</year></date>
           <date date-type="accepted"><day>29</day><month>August</month><year>2017</year></date>
      </history>
      <permissions>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions><self-uri xlink:href="https://nhess.copernicus.org/articles/.html">This article is available from https://nhess.copernicus.org/articles/.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/.pdf</self-uri>


      <abstract>
    <p>A big challenge in terms or landslide risk mitigation is represented by
increasing the resiliency of society exposed to the risk. Among the
possible strategies with which to reach this goal, there is the implementation of
early warning systems. This paper describes a procedure to improve early warning
activities in areas affected by high landslide risk, such as those
classified as critical infrastructures for their central role in society.</p>
    <p>This research is part of the project “LEWIS (Landslides Early Warning
Integrated System): An Integrated System for Landslide Monitoring, Early
Warning and Risk Mitigation along Lifelines”.</p>
    <p>LEWIS is composed of a susceptibility assessment methodology providing
information for single points and areal monitoring systems, a data
transmission network and a data collecting and processing center (DCPC),
where readings from all monitoring systems and mathematical models converge
and which sets the basis for warning and intervention activities.</p>
    <p>The aim of this paper is to show how logistic issues linked to advanced
monitoring techniques, such as big data transfer and storing, can be dealt
with compatibly with an early warning system. Therefore, we focus on the
interaction between an areal monitoring tool (a ground-based interferometric
radar) and the DCPC. By converting complex data into ASCII strings and
through appropriate data cropping and average, and by implementing an
algorithm for line-of-sight correction, we managed to reduce the data daily
output without compromising the capability for performing.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p>Urbanization, especially in mountain areas, can be considered a major cause
for high landslide risk because of the increased exposure of elements at
risk. Among the elements at risk, important communication routes, such as
highways, can be classified as critical infrastructures (CIs), since their
rupture can cause chain effects with catastrophic damages on society
(Geertsema et al., 2009; Kadri et al., 2014). On the other hand, modern
society is more and more dependent on CIs and their continuous efficiency
(Lebaka et al., 2016), and this has increased their value over the years. The
result is a higher social vulnerability in the face of loss of continuous
operation (Kröger, 2008). The main objective was to improve the social
preparedness for the growing landslide risk, according to the suggestions of
several authors (Gene Corley et al., 1998; Baldridge and
Marshall, 2011; Urlainis et al., 2014, 2015). This led to the development
of several approaches and frameworks for increasing the resiliency of society
exposed to the risk (Kröger, 2008; Cagno et al., 2011, and references
therein). The resiliency policy involves not only prevention activities but
also, and more importantly, those activities needed to maintain functionality
after disruption (Snyder and Burns, 2009) and to promptly alert people of incoming
catastrophes in order to protect them and prepare for a possible damaging
of the endangered CI. Among these activities, the implementation of
integrated landslides early warning systems (i.e., LEWIS: Landslides Early Warning
Integrated System: An Integrated System for Landslide Monitoring, Early
Warning and Risk Mitigation along Lifelines; Versace et al.,
2012; Costanzo et al., 2016) reveals its increasing importance.</p>
      <p>In this context, the methodology described in this paper has been conceived;
it has been tested and validated on a portion of an Italian highway that is
affected by landslides and that was selected as a case study: it is located in southern
Italy, along a section of the A16 highway, an important communication route
that connects Naples to Bari, where a ground-based interferometric synthetic
aperture radar (GB-InSAR) has been installed at the test site in order to
obtain spatial monitoring data.</p>
      <p>One of the main drawbacks of advanced instruments such as GB-InSAR is how to
handle the large data flow deriving from continuous real-time monitoring.
The issue is to reduce the capacity needed for analyzing, transmitting and
storing big data without losing important information. The main feature of
this paper is indeed the management of monitoring data in order to filter,
correct, transfer and access them compatibly with the needs of an early warning system.</p>
</sec>
<sec id="Ch1.S2">
  <title>Materials and methods</title>
<sec id="Ch1.S2.SS1">
  <title>GB-InSAR</title>
      <p>The GB-InSAR is composed of a microwave transceiver mounted on a linear rail
(Tarchi et al., 1997; Rudolf et al., 1999; Tarchi et al., 1999). The system
used is based on a continuous-wave–stepped-frequency radar, which moves
along the rail at millimeter steps in order to perform the synthetic
aperture: the longer the rail, the higher the cross-range resolution. The
microwave transmitter produces, step by step, continuous waves around a
central frequency, which influences the cross-range resolution and
determines the interferometric sensitivity, i.e., the minimum measurable
displacement, usually largely smaller than the corresponding wavelength.</p>
      <p>The radar produces complex radar images containing the information relative
to both phase and amplitude of the microwave signal backscattered by the
target (Bamler and Hartl, 1998; Antonello et al., 2004). The amplitude of a
single image provides the radar reflectivity of the scenario at a given
time, while the phase of a single image is not usable. The technique that
enables to retrieve displacement information is called interferometry and
requires the phase from two images. In this way, it is possible to elaborate
a displacement map relative to the elapsed time between the two
acquisitions.</p>
      <p>The main added value of GB-InSAR is its capability to blend the boundary
between mapping and monitoring, by computing 2-D displacement maps in near-real
time. The use of this tool to monitor structures, landslides, volcanoes and
sinkholes is widely documented (Calvari et al., 2016; Di Traglia, 2014;
Intrieri et al., 2015; Bardi et al., 2016, 2017; Martino and Mazzanti, 2014;
Severin et al., 2014; Tapete et al., 2013), as well as for early
warning and forecasting (Intrieri et al., 2012; Carlà et al., 2016a, b;
Lombardi et al., 2016).</p>
      <p>GB-InSAR systems probably reveal their full potential in emergency
conditions. They are transportable and only require from a few tens of minutes
to a few hours to be installed (depending on the logistics of the site).
Moreover, they can detect “near-real-time” area displacements, without
accessing the unstable area, 24 h a day and in all weather conditions (Del
Ventisette et al., 2011; Luzi, 2010; Monserrat et al., 2014). On the other
hand, some limitations reduce the GB-InSAR technique applicability: first of
all, the scenario must present specific characteristics in order to reflect
microwave radiations, maintaining high coherence values (Luzi, 2010;
Monserrat et al., 2014); only a component of the real displacement vector can
be identified (i.e., the component parallel to the sensor's line of sight);
and maximum detectable velocities are connected to the time that the system needs
to obtain two subsequent acquisitions. Sensors need power supply that, for
long-term monitoring, cannot be replaced by batteries, generators or solar
panels.</p>
      <p>With the specific aim of performing the function of an early warning system,
data acquired
in situ must be sent automatically to a “control center” where they are
integrated into a complete early warning system procedure (Intrieri et al.,
2013). In this sense, another main limitation is represented by the necessity
to transfer a high quantity of data, whose weight has to be reduced to the
minimum, in order to reduce the load on transmission network.</p>
      <p>The employed system is a portable device designed and implemented by the
Joint Research Center (JRC) of the European Commission and its spin-off
company Ellegi-LiSALab (Tarchi et al., 2003; Antonello et al., 2004).</p>
</sec>
<sec id="Ch1.S2.SS2">
  <title>Early warning system architecture</title>
      <p>Morphological features, hydrogeological factors and sudden rainfall can
cause diverse types of movements or fall of earthy and rock materials. The
unpredictability and diversity of these events make structural interventions
often inappropriate to reduce the related risk and a real-time monitoring
network difficult to implement.</p>
      <p>In the last decade, wireless sensor networks (WSNs) have been used
extensively in various fields. A significant increase in the use of WSNs – due to their
simplicity and the low cost of installation, manufacturing and maintenance – has
been recorded in the framework of environmental monitoring applications
(Intrieri et al., 2012; Liu et al., 2007; Yoo et al., 2007). Distinct types
of sensor nodes of these networks, distributed with high density in the
monitored areas, send environmental information to the concentrators nodes,
generating a considerable amount and a wide variety of collected data. Due
to the significant growth of data volumes to be transferred, the WSNs require
flexible ad hoc protocols able to respect constraints related to energy
consumption management (Hadadian and Kavian, 2016; Khaday et al., 2015;
Parthasarathy et al., 2015). In particular, many protocols have been
developed that offer data aggregation patterns to optimize the sensor nodes'
battery life (Kim et al., 2015) or sleep–measurement–data transfer cycles to
minimize the energy consumption (Fei et al., 2013; Venkateswaran and
Kennedy, 2013).</p>
      <p>LEWIS (Costanzo et al., 2016) uses heterogeneous sensors, distributed in the
risk areas, to monitor the several physical quantities related to landslides.
The measured data, through a telecommunications network, flow into the data
collecting and processing center (DCPC), where, using suitable mathematical
models for the monitored site, the risk is evaluated and eventually the state
of alert for mitigation action is released (Fig. 1).</p>
      <p>The system, through a modular architecture exploiting a telecommunication
network (called LEWARnet) based on an ad hoc communication protocol and an
adaptive middleware, has a high flexibility, which allows for the use of
different interchangeable technological solutions to monitor the parameters
of interest.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><caption><p>LEWIS architecture.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f01.png"/>

        </fig>

      <p>The network has been equipped with both single-point sensors and area
sensors. The present paper addresses a sub-network comprising an area
sensor, the GB-InSAR.</p>
      <p>The different sensors types generate asynchronous traffic, thus imposing the
adoption of an ad hoc transmission protocol. This can support an
asynchronous transmission mode to the DCPC, and it is equipped with message
queue management capacity to reconstruct historical data series, between
two connection sessions, in case of null or partial transmission. This
operation mode requires the presence of a software architecture that
operates as a buffer, acting as an intermediary or as middleware (LEWARnet)
between the data consumer (DCPC) and the data producers (sensors and
sub-networks of sensors).</p>
      <p>The developed middleware also monitors the processes of transmission and
data acquisition, recognizing the activity status of the sensors and that of
the DCPC, and integrating encryption and data compression functions.</p>
      <p>A detailed description of LEWIS can be found in Costanzo et al. (2015, 2016).</p>
</sec>
<sec id="Ch1.S2.SS3">
  <title>Data collecting and processing center</title>
      <p>The management of information flows, the telematic architecture and the
services for data management are entrusted to the DCPC.</p>
      <p>The DCPC has been designed and performed according to a complex hardware and
software system able to ensure the reliability and continuity of the
service, providing advance information of possible dangerous situations that
may occur.</p>
      <p>In the research project, the DCPC has to ensure the continuous exchange of
information among monitoring networks, mathematical models and the command
and control center (CCC) that is responsible for emergency management and
decision making.</p>
      <p>Data flow from the monitoring network was managed according to a
communication protocol implemented by the DCPC and named AqSERV. AqSERV was
designed considering the heterogeneity of devices of monitoring and
transmission networks (single-point and area sensors) and the available
hardware resources (microcontrollers and/or industrial computers). AqSERV was
devised to link the DCPC database (named LEWISDB) to the monitoring networks,
after validation of the authenticity of the node that connects to the
center. Data acquisition, before the storage in the database, is validated
both syntactically and according to the information content. The procedures
for extraction of the information content and validation have been realized
differently for single-point and area sensors: the latter require a more
complex validation, as they work in a 2-D domain.</p>
      <p>The complete management of the monitoring networks by DCPC has been realized
through specific remote commands, sent to individual devices via AqSERV, to
reconfigure the acquisition intervals or to activate any sensor, depending
on the natural phenomena occurring in real time.</p>
      <p>The configuration of monitoring networks – composed of devices and sensors,
of communication protocol used by each network, and of rules for extraction
and validation of information content – is carried out through a Web
application that allows for the management of the entire system by the
users.</p>
      <p>The real-time search for acquisitions is carried out through a WebGIS that
has been specifically designed for WSNs but that can be easily extended to classic
monitoring networks.</p>
      <p>The WebGIS was designed according to the traditional Web architecture,
client–server, by using network services which are Web mapping oriented:
<list list-type="bullet"><list-item>
      <p>Web server for static data,</p></list-item><list-item>
      <p>Web server for dynamic data,</p></list-item><list-item>
      <p>server for maps,</p></list-item><list-item>
      <p>database for the management of map data.</p></list-item></list></p>
</sec>
</sec>
<sec id="Ch1.S3">
  <title>Test site</title>
      <p>The test site chosen to experiment the integrated system is located in
southern Italy, along a section of the A16 highway, an important
communication route that connects Naples to Bari (Fig. 2). The selected
section of the A16 highway runs in the SW–NE direction, along the southern Italian Apennines, in
correspondence with the valley of the Calaggio Creek, between the towns of
Lacedonia (Campania region) and Candela (Puglia region).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><caption><p>Landslides detected through field survey along the monitored section
of A16 highway.</p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f02.png"/>

      </fig>

      <p>The area is tectonically active, but the landscape, characterized by gentle
slopes, is mostly influenced by lithologic factors rather than by tectonics.
The lithologies outcropping in this area are Pliocene–Quaternary clay, clayey
marlstones and more recent (Holocene) terraced alluvial sediments (from clay
to gravel). The landslides shown in Fig. 2 are all located in clay or clayey
marlstones.</p>
      <p>The highway runs on the right flank of the Calaggio Creek at an altitude
between 300 and 400 m a.s.l.; the section of interest represents an element
at risk in the computation of landslide risk assessment, due to the presence
of unstable areas which can potentially affect the communication route
(Fig. 2). These unstable areas mainly involve clayey superficial layers.</p>
      <p>On 1 July 2014, the GB-InSAR system was installed on the test site. The
location of the installation point was selected, taking into account the view
of the unstable area and the distance from the power supply network. A
covered structure was built to protect the system from atmospheric agents and
possible acts of vandalism, in the perspective of a long-term monitoring.</p>
      <p>The transmission network was provided by a GSM modem, exploiting the 3G
network. In addition to the PC integrated into the GB-InSAR power base, a
further external PC was exclusively employed for data after elaboration and
transmission.</p>
      <p>The system acquired data from the beginning of July 2014 until the end of July
2015.</p>
      <p>The installation location allowed the system to detect an area between 40 and
400 m from the its position in the range direction and about 360 m wide in
the azimuth direction. These values, coupled with a 40<inline-formula><mml:math id="M1" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> vertical
aperture of the antennas, allowed operators to detect an area of about
360 m <inline-formula><mml:math id="M2" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 360 m.</p>
</sec>
<sec id="Ch1.S4">
  <title>Data management</title>
      <p>The most relevant matter of this monitoring was not as much related to the
detection of landslide movements threatening the highway as to how
long-term monitoring performed with an instrument providing huge amounts of
data could have been run without resorting to large hard drives or to fast
Internet connections. In fact, the monitoring area was covered by a 3G
mobile telecommunication networks with a limit of 2-gigabyte data transfer
per month, and there was the need to reduce the massive data flow produced by
the radar.</p>
      <p>For this reason, an appropriate data management system (Fig. 3) was developed and is
described herein.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3"><caption><p>Diagram showing the complete data flow from acquisition to final
visualization.</p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f03.png"/>

      </fig>

<sec id="Ch1.S4.SS1">
  <title>Data acquisition</title>
      <p>The GB-InSAR employed produced a single radar image, consisting of a <inline-formula><mml:math id="M3" display="inline"><mml:mrow><mml:mn mathvariant="normal">1001</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">1001</mml:mn></mml:mrow></mml:math></inline-formula> complex matrix, every 5 min. Each one is around 8 megabytes
large, resulting in more than 2 gigabytes of data produced every day.</p>
      <p>This amount of data represented an issue for both store capacity and data
transmission.</p>
</sec>
<sec id="Ch1.S4.SS2">
  <title>Data elaboration</title>
      <p>After being acquired, data were then transferred through LAN connection to
the external PC implementing a dedicated Matlab script locally performing
the actions described as follows.</p>
<sec id="Ch1.S4.SS2.SSS1">
  <title>Data averaging</title>
      <p>In order to reduce the noise normally affecting radar data (especially in
vegetated areas), the images acquired every 5 min were also averaged using
all data of the previous 8 and 24 h. Then images averaged over 24 h were
used to calculate daily displacement maps every 8 h to create 8 h
displacement maps, and non-averaged images were used to calculate 5 min displacement
maps. These time frames were selected based on the characteristics of
the slope movements and signal / noise ratio in the investigated area.</p>
      <p>Averaging is also a way to make good use of a high data frequency, since
it enables the memory occupied in the database to be reduced as an alternative
to their direct elimination.</p>
</sec>
<sec id="Ch1.S4.SS2.SSS2">
  <title>Displacement map calculation and ASCII conversion</title>
      <p>Each radar image can be represented as in Eq. (1):
              <disp-formula id="Ch1.E1" content-type="numbered"><mml:math id="M4" display="block"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>n</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msub><mml:mi>A</mml:mi><mml:mi>n</mml:mi></mml:msub><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>exp⁡</mml:mi><mml:mo>(</mml:mo><mml:mi>j</mml:mi><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mi>n</mml:mi></mml:msub><mml:mo>)</mml:mo><mml:mi>m</mml:mi></mml:mrow></mml:math></disp-formula>
            where <inline-formula><mml:math id="M5" display="inline"><mml:mrow><mml:msub><mml:mi>A</mml:mi><mml:mi>n</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the amplitude of the <inline-formula><mml:math id="M6" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula>th image, <inline-formula><mml:math id="M7" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mi>n</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is its phase
and <inline-formula><mml:math id="M8" display="inline"><mml:mrow><mml:mi>j</mml:mi><mml:mo>=</mml:mo><mml:mo>(</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:msup><mml:mo>)</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> is the imaginary unit. The displacement <inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>r</mml:mi></mml:mrow></mml:math></inline-formula>
occurred in the time period between the acquisition of <inline-formula><mml:math id="M10" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
was calculated with the following (Eq. 2):
              <disp-formula id="Ch1.E2" content-type="numbered"><mml:math id="M12" display="block"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>r</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mo>=</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mo>(</mml:mo><mml:mi mathvariant="italic">λ</mml:mi><mml:mo>/</mml:mo><mml:mn mathvariant="normal">4</mml:mn><mml:mi mathvariant="italic">π</mml:mi><mml:mo>)</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>⋅</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi mathvariant="italic">φ</mml:mi><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
            where <inline-formula><mml:math id="M13" display="inline"><mml:mi mathvariant="italic">λ</mml:mi></mml:math></inline-formula> is the wavelength of the signal and
              <disp-formula id="Ch1.E3" content-type="numbered"><mml:math id="M14" display="block"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi mathvariant="italic">φ</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>=</mml:mo><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>-</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></disp-formula>
            can be derived from
              <disp-formula id="Ch1.E4" content-type="numbered"><mml:math id="M15" display="block"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>=</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msubsup><mml:mi>S</mml:mi><mml:mn mathvariant="normal">2</mml:mn><mml:mo>∗</mml:mo></mml:msubsup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>=</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msub><mml:mi>A</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:msub><mml:mi>A</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>exp⁡</mml:mi><mml:mo>[</mml:mo><mml:mi>j</mml:mi><mml:mo>(</mml:mo><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mo>-</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msub><mml:mi mathvariant="italic">φ</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>]</mml:mo><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula>
            As a result, an ASCII file was obtained that only contains the information relative to the
displacement for each pixel.</p>
</sec>
<sec id="Ch1.S4.SS2.SSS3">
  <title>Atmospheric correction</title>
      <p>One of the major advantages of GB-InSAR is the capability to achieve
sub-millimeter precision. However, this can be severely hampered by the
variations of air temperature and humidity, especially when long distances
are involved. Usually, atmospheric correction is performed by choosing one
area considered stable, taking into account that every displacement value
different from 0 is due to atmospheric noise and assuming that this offset is
a linear function of the distance. Based on this relation the
entire displacement map is corrected. In our case the whole scenario has been
selected, and then only the potentially unstable zones and those with a weak or
incoherent backscattered signal were removed. The remaining areas were then
considered stable and therefore were used for calculating the atmospheric
effects. This results in a larger correction region that enables a
statistical correlation between the atmospheric effects and the distance and
therefore the calculation of a site-specific regression function that may not
necessarily be linear (Fig. 4).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><caption><p>The color bar is expressed in millimeters; green indicates stable pixels,
while blue and red respectively indicate movement toward and away from the GB-InSAR.
<bold>(a)</bold> Raw interferogram showing artificial displacement increasing
linearly with distance (as typical of atmospheric noise). <bold>(b)</bold> The
same interferogram after the atmospheric correction.</p></caption>
            <?xmltex \igopts{width=497.923228pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f04.png"/>

          </fig>

</sec>
<sec id="Ch1.S4.SS2.SSS4">
  <title>Line-of-sight correction</title>
      <p>The availability to detect only the line-of-sight (LOS) component of the
displacement vector represents one of the main limitations of the GB-InSAR
technique. A method to partially overcome this limitation has been applied in
this paper, following the procedure described in Colesanti and Wasowski
(2006) and later in Bardi et al. (2014, 2016). Other methods have been
employed by Cascini et al. (2010, 2013).</p>
      <p>Assuming the downslope direction as the most probable displacement path,
radar data have been projected in this direction. Input data as the angular
values of the aspect and slope have been derived from the
digital terrain model (DTM) of the investigated area;
furthermore, azimuth angle and incidence angle of the radar LOS have been
obtained.</p>
      <p>After calculating the direction cosines of LOS and slope (respectively
functions of azimuth and incidence angles and aspect and slope angles) in the
directions of zenith (<inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M17" display="inline"><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, north
(<inline-formula><mml:math id="M18" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M19" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> and east (<inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>,
<inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, the coefficient <inline-formula><mml:math id="M22" display="inline"><mml:mi>C</mml:mi></mml:math></inline-formula> is defined as follows (Eq. 5):
              <disp-formula id="Ch1.E5" content-type="numbered"><mml:math id="M23" display="block"><mml:mrow><mml:mi>C</mml:mi><mml:mo>=</mml:mo><mml:msub><mml:mi>Z</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>Z</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>N</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>N</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>E</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>E</mml:mi><mml:mi mathvariant="normal">slope</mml:mi></mml:msub><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula>
            <inline-formula><mml:math id="M24" display="inline"><mml:mi>C</mml:mi></mml:math></inline-formula> represents the percentage of real displacement detected by the radar
sensor (Fig. 5a).</p>
      <p>The real displacement (<inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mi mathvariant="normal">real</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> is defined as the ratio between the
displacement recorded along the LOS (<inline-formula><mml:math id="M26" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mi mathvariant="normal">los</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> and the <inline-formula><mml:math id="M27" display="inline"><mml:mi>C</mml:mi></mml:math></inline-formula> value
(Fig. 5b).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><caption><p><bold>(a)</bold> <inline-formula><mml:math id="M28" display="inline"><mml:mi>C</mml:mi></mml:math></inline-formula> values map. Blue arrows indicate the downslope
direction. <bold>(b)</bold> Cumulated displacement values projected in the
downslope direction, referring to a period between 1 July and 1 November 2014.
The yellow asterisk on the left of the images represents the location of the
GB-InSAR.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f05.png"/>

          </fig>

      <p>Assuming that the studied landslide actually moves in the downslope
direction, the GB-InSAR detectable real displacement percentage ranges
between 22 and 60 % (Fig. 5a).</p>
      <p>In Fig. 5b, an example of a slope displacement map is shown. Here,
cumulated displacement data related to a period between 1 July and 1 November
2014 have been projected in the downslope direction. Data show that the area
can be considered stable in the referred period; maximum displacement values
of 4 mm in 4 months (eastern portion of observed scenario) can be still
considered in the range of stability.</p>
</sec>
<sec id="Ch1.S4.SS2.SSS5">
  <title>Time series extraction</title>
      <p>In order to allow for a fast data transfer–velocity threshold comparison,
some representative control points were selected, aimed at providing
cumulated displacement time series. Control points were retrieved from the
same displacement maps calculated as described in Sect. 5.2.2 and therefore
can be relative to a time frame of 5 min, 8 h or 24 h.</p>
      <p>In the case of noisy data, instead of having a time series relative to a single
pixel, these can be retrieved from a spatial average obtained from a small
area consisting of few pixels.</p>
</sec>
<sec id="Ch1.S4.SS2.SSS6">
  <title>Scenario cropping</title>
      <p>Typically, the field of view of a GB-InSAR is larger than the actual area to
be monitored. In fact, a portion of the radar image may be relative to the
ground, sky and areas geometrically shadowed or covered by dense vegetation.
These may be of no interest or even contain no information at all. For the
case here studied around 50 % of a radar image had a low coherence and
was for all practical purposes unusable. Therefore, a cropping of the ASCII
displacement map occurred in order to frame only the relevant area.</p>
</sec>
</sec>
<sec id="Ch1.S4.SS3">
  <title>Data transfer and visualization</title>
      <p>The interferometric data generated by GB-InSAR, after the pre-processing and
proper correction previously described, are ready for transfer to the DCPC.
The transmission of these data to the DCPC is mediated by the middleware,
which interrogates the GB-InSAR in order to track the state, detects the newest
data, and reorders and marks them to properly build data time series to be
transferred to DCPC.</p>
      <p>Subsequently, the middleware manages communications with the DCPC, according
to the implemented ad hoc protocol. This ensures the security of data
providers through encrypted authentication mechanisms; it allows for
recovering missing or partially transmitted data, thus avoiding information
loss; and it provides data acquired by the sensors to the DCPC in a
standardized format, JSON, able to guarantee uniformity between the various
information provided by the various sensors types. All these particular
features fully justify the adoption of an ad hoc protocol for data transfer,
instead of using a standard protocol such as FTP.</p>
      <p>The data files produced by the GB-InSAR have already been locally
pre-processed and result in a matrix expressed in ASCII code; the dimensions
of the matrix are known and range from <inline-formula><mml:math id="M29" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula> (for the displacement of
single control points) to <inline-formula><mml:math id="M30" display="inline"><mml:mrow><mml:mn mathvariant="normal">1001</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">1001</mml:mn></mml:mrow></mml:math></inline-formula> (for uncropped displacement
maps). Before encapsulating these data in the message to be transferred to
DCPC, the middleware converts them from ASCII code to character strings,
using the standard coding ISO/IEC 8859-1, and so is able to obtain a data
compression with a factor equal to <inline-formula><mml:math id="M31" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">8</mml:mn></mml:mrow></mml:math></inline-formula>.</p>
      <p>Eventually the DCPC is entrusted with cumulating the displacements relative
to the control points, which are compared with the respective thresholds,
and with visualizing the displacement maps as WebGIS layers, thus enabling
data validation and the evaluation of the extension of moving surface.</p>
</sec>
</sec>
<sec id="Ch1.S5">
  <title>Early warning procedure discussions</title>
      <p>The GB-InSAR is part of a larger early warning system (LEWIS) which also
includes other monitoring systems and simulation models. Therefore, to
understand how GB-InSAR data can be used in an early warning context, it
is necessary to make reference to LEWIS as a whole.</p>
      <p>Any information coming from the investigated sites and subsequently
processed also by using the simulation models is used to define an
intervention model. This is based on the following elements: event
scenarios, risk scenarios, levels of criticality and levels of alert.</p>
      <p>Event scenarios describe the properties of expected phenomena in terms of
dimension, velocity, involved material and occurrence probability. Occurrence
probability depends on the associated time horizon, which should be equal to
a few hours at most, in the case of early warning systems. Evaluation of
occurrence probability is carried out by using information from monitoring
systems and/or from outputs of adopted mathematical models for nowcasting.
All the properties to be analyzed for event scenarios are listed below; a
subdivision in classes is adopted for each one:
<list list-type="bullet"><list-item>
      <p>landslide velocity (five classes from slow to extremely rapid);</p></list-item><list-item>
      <p>landslide surface (five classes from very small to very large);</p></list-item><list-item>
      <p>landslide scarp (five classes from very small to very large);</p></list-item><list-item>
      <p>landslide volume (five classes from extremely small to large);</p></list-item><list-item>
      <p>thickness (five classes from very shallow to very deep);</p></list-item><list-item>
      <p>magnitude (three classes: low, moderate, high), which combines the previous information;</p></list-item><list-item>
      <p>involved material (mud, debris, earth, rock, mixture of components);</p></list-item><list-item>
      <p>occurrence probability (zero, low, moderate, high, very high, equal to 1).</p></list-item></list>
While some of the aforementioned parameters are determined by geological
surveys, landslide velocity is directly derived from monitoring data (such as
those collected by GB-InSAR). Landslide surface can be determined by
geomorphological observation but is precisely quantified by GB-InSAR, thanks
to its capability to produce 2-D displacement maps.</p>
      <p>Risk scenarios can be firstly grouped in the following three classes:
<list list-type="custom"><list-item><label>A.</label>
      <p>mud and/or debris movements which could induce a friction reduction
between the vehicles and the tar and therefore facilitate slips;</p></list-item><list-item><label>B.</label>
      <p>road subsidence induced by landslides that could drag or drop vehicles;</p></list-item><list-item><label>C.</label>
      <p>falls of significant volumes and/or boulders that could crush or cover
vehicles and constitute an obstacle for other vehicles.</p></list-item></list>
For each previous risk scenario, six sub-scenarios can be identified based on
the number of potentially involved infrastructures, carriageways and lanes
(a: hydraulic infrastructures
and/or barriers of either carriageway; b: only the emergency lane of either carriageway;
c: the emergency lane and up to the regular lane of either carriageway;
d: up to the fast lane of either carriageway; e: up to the fast lane of the opposite carriageway;
f: up to the regular lane of the opposite carriageway).
Thus, the total number of possible risk scenarios is 18 (Fig. 6), indicated
with a couple of letters (capital and small).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6"><caption><p>Top and middle: possible risk scenarios involving scenario A
(landslides that could reduce friction) to increasing sectors of the highway.
Bottom: combinations of scenarios with several types of phenomena that
affect the emergency lane, regular lane and fast lane.</p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://nhess.copernicus.org/articles/17/1713/2017/nhess-17-1713-2017-f06.png"/>

      </fig>

      <p>The following information is provided to DCPC:
<list list-type="bullet"><list-item>
      <p>measurements from sensors,</p></list-item><list-item>
      <p>model outputs,</p></list-item></list>
and four states are identified for each of them:
<list list-type="bullet"><list-item>
      <p>state 0: no variation,</p></list-item><list-item>
      <p>state 1: small variation,</p></list-item><list-item>
      <p>state 2: moderate variation,</p></list-item><list-item>
      <p>state 3: high variation.</p></list-item></list>
In practice, for the GB-InSAR, such states are delimited by fixed velocity
values (thresholds). In this application values have been selected according
to the gathered data, the first threshold being just above the instrumental
noise; the remaining have been set based on expert judgement waiting for a
more robust calibration, which is possible only after at least a partial
mobilization of the slope. Anyway, the system is open to any method for
determining thresholds (Crosta and Agliardi, 2003; Du et al., 2013;
Carlà et al., 2016a) and also to the use of other parameters
(acceleration for example).</p>
      <p>Besides information from sensors and models, other information is obtained
from meteorological and hydrological models (named “indicators”).</p>
      <p>Indicators comprise weather forecasting and output of the Forecasting of
Landslides Induced by Rainfall (FLaIR) and Saturated Unsaturated Simulation
for Hillslope Instability (SUSHI) models (Sirangelo et al., 2003; Capparelli
and Versace, 2011) on the basis of observed and predicted (for the successive
6 h) rainfall heights.</p>
      <p>Two states are defined for indicators:
<list list-type="bullet"><list-item>
      <p>state 0: no variation or not significant,</p></list-item><list-item>
      <p>state 1: significant variation.</p></list-item></list>
To sum up, DCPC has the following information at any moment:
<list list-type="bullet"><list-item>
      <p>state (0, 1) of indicators (INDs),</p></list-item><list-item>
      <p>state (0, 1, 2, 3) of sensors and models running for the specific highway
section (SEN),</p></list-item></list>
and, on the basis of these states, four different decisions can be made by
DCPC, one of which with three options.</p>
      <p>All the possible decisions are illustrated in Table 1, in which the weight of
the several sensors is assumed to be the same. Based on the notices of
criticality levels provided by the DCPC, and on its own independent
evaluations, the CCC issues the appropriate warning notices (surveillance,
alert, alarm and warning) and makes decisions about the consequent actions.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><caption><p>DCPC possible decisions.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="2">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="224pt"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:thead>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">State of sensors and/or models</oasis:entry>  
         <oasis:entry colname="col2">DCPC decisions</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">All INDs and SENs are S0</oasis:entry>  
         <oasis:entry colname="col2">0 – no decision</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">At least one IND is S1 and all SENs are S0</oasis:entry>  
         <oasis:entry colname="col2">1 – sensor on demand activation</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">At least one SEN is S1</oasis:entry>  
         <oasis:entry colname="col2">2 – to intensify the presence up to 24 h a day</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">At least <inline-formula><mml:math id="M32" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula> SENs are S1 or at least one SEN is S2</oasis:entry>  
         <oasis:entry colname="col2">3/1 – to issue a notice of ordinary criticality (level 1)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">At least <inline-formula><mml:math id="M33" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula> SENs are S2 or at least one SEN is S3</oasis:entry>  
         <oasis:entry colname="col2">3/2 – to issue a notice of moderate criticality (level 2)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">At least <inline-formula><mml:math id="M34" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula> SENs are S3</oasis:entry>  
         <oasis:entry colname="col2">3/3 – to issue a notice of high or severe criticality (level 3)</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p>The information of each sensor and the results produced by the models are
used to assess, in each instant, the occurrence probability of an event
scenario in the monitored areas and the possible risk scenarios.</p>
      <p>This combination of heterogeneous data was carried out by identifying for
each sensor and model typical information (displacement, precipitation,
inclination etc.); evaluating the state at each instant, according to a
threshold system; and combining this result for all sensors placed in a
monitored geomorphological area.</p>
      <p>The result is constituted by the occurrence probability of an event
scenario, which is associated with a specific action by the DCPC. In
particular, if the occurrence probability is low, moderate or high, it is
necessary to issue a notice of criticality (ordinary – level 1; moderate –
level 2; high – level 3) to the CCC.</p>
      <p>The DCPC sends two types of information:
<list list-type="order"><list-item>
      <p>criticality state of the single monitored geomorphological unit,</p></list-item><list-item>
      <p>criticality state of the whole area.</p></list-item></list>
The adopted communication protocol between the two centers for the exchange
of information was carried out through a Web service provided by the CCC,
using the classes and attributes of the methodology named DATEX II (which is
a protocol for the exchange of traffic data). The use of the Web service
allowed ensuring the interoperability of data between the two centers,
regardless of the hardware and software architecture used, through a
persistent service capable of ensuring an immediate restoration of the
connections, in case of malfunction, and a continuous monitoring between the
two centers, even in the absence of criticality.</p>
</sec>
<sec id="Ch1.S6" sec-type="conclusions">
  <title>Conclusions</title>
      <p>The GB-InSAR is a monitoring tool that is becoming more and more used in
landslide monitoring and early warning, especially thanks to its capability
to produce real-time, 2-D displacement maps. On the other hand, it still
suffers from some drawbacks, such as the limitation of measuring only the
LOS component of a target's movement and logistic issues like those owing to
a massive production of data that may cause trouble for both storing
capacity and data transfer. In particular, the latter is a more and more
common problem of advanced technologies that are able to produce high-quality
data with a high acquisition frequency, which may leave the problem
of finding the balancing between exploiting all the information and at the same
time avoiding unnecessary redundancy.</p>
      <p>These problems were addressed when a GB-InSAR was integrated within a
complex early warning system (LEWIS) and only a limited Internet connection
was available. This situation required that a series of pre-elaboration
processes and data management procedures take place in situ in order to
produce standardized and reduced files, carrying only the information needed
when it was needed. The procedures mainly concerned the transmission of data
averaged over determined time frames, proportionate with the kinematics of
the monitored phenomenon. Previously, transmission data were also corrected
(in terms of both atmospheric noise and LOS) and reduced, by filtering out
the information relative to the amplitude of the targets, by eliminating the
areas not relevant for the monitoring and by transforming the matrices into
strings.</p>
      <p>As a result, GB-InSAR data converged into the early warning system and
contributed to it by producing displacement time series of representative
control points to be compared with fixed thresholds. Displacement maps were
also available for data validation by expert operators and for retrieving
information relative to the surface of the moving areas.</p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability">

      <p>The present paper concerns a methodology. Some of the data used in this paper are no longer available; the remaining
available data can be requested from the corresponding author.</p>
  </notes><notes notes-type="competinginterests">

      <p>The authors declare that they have no conflict of interest.</p>
  </notes><notes notes-type="sistatement">

      <p>This article is part of the special issue “Landslide early warning systems:
monitoring systems, rainfall thresholds, warning models, performance evaluation and risk perception”.
It is not associated with a conference.</p>
  </notes><ack><title>Acknowledgements</title><p>This research is part of the project “LEWIS (Landslides Early Warning
Integrated System): An Integrated System for Landslide Monitoring, Early
Warning and Risk Mitigation along Lifelines”, financed by the Italian
Ministry of Education, Universities and Research and co-funded by the
European Regional Development Fund, in the framework of the National
Operational Programme 2007–13 “Research and Competitiveness”, grant
agreement no. PON01_01503.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>The authors are thankful to Giuseppe Della Porta and his colleagues from
Autostrade S.p.A. for their availability in permitting and supporting the
installation and maintenance of the GB-InSAR along the A16 highway.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>
Edited by: Stefano Luigi Gariano<?xmltex \hack{\newline}?>
Reviewed by: two anonymous referees</p></ack><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><mixed-citation>
Antonello, G., Casagli, N., Farina, P., Leva, D., Nico, G., Sieber, A. J.,
and Tarchi, D.: Ground-based SAR interferometry for monitoring mass
movements, Landslides, 1, 21–28, 2004.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><mixed-citation>Baldridge, S. M. and Marshall, J. D.: Performance of structures in the January
2010 MW 7.0 Haiti earthquake, Structures Congress, 1660–1671, <ext-link xlink:href="https://doi.org/10.1061/41171(401)145" ext-link-type="DOI">10.1061/41171(401)145</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><mixed-citation>
Bamler, R. and Hartl, P.: Synthetic Aperture Radar Interferometry, Inverse
Probl., 14, R1–R54, 1998.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><mixed-citation>
Bardi, F., Frodella, W., Ciampalini, A., Del Ventisette, C., Gigli, G.,
Fanti, R., Basile, G., Moretti, S., and Casagli, N.: Integration between
ground based and satellite SAR data in landslide mapping: The San Fratello
case study, Geomorphology, 223, 45–60, 2014.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><mixed-citation>Bardi, F., Raspini, F., Ciampalini, A., Kristensen, L., Rouyet, L., Lauknes,
T. R., Frauenfelder, R., and Casagli, N.: Space-Borne and Ground-Based InSAR
Data Integration: The Åknes Test Site, Remote Sens.-Basel., 8, 237, <ext-link xlink:href="https://doi.org/10.3390/rs8030237" ext-link-type="DOI">10.3390/rs8030237</ext-link>,
2016.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><mixed-citation>Bardi, F., Raspini, F., Frodella, W., Lombardi, L., Nocentini, M., Gigli,
G., Morelli, S., Corsini, A., and Casagli, N.: Monitoring the Rapid-Moving
reactivation of Earth Flows by Means of GB-InSAR: The April 2013 Capriglio
Landslide (Northern Appennines, Italy),
Remote Sens.-Basel., 9, 165, <ext-link xlink:href="https://doi.org/10.3390/rs9020165" ext-link-type="DOI">10.3390/rs9020165</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><mixed-citation>
Cagno, E., De Ambroggi, M., Grande, O., and Trucco, T.: Risk analysis of
underground infrastructures in urban areas, Reliab. Eng. Syst. Safe, 96,
139–148, 2011.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><mixed-citation>Calvari, S., Intrieri, E., Di Traglia, F., Bonaccorso, A., Casagli, N., and
Cristaldi, A.: Monitoring crater-wall collapse at active volcanoes: a study
of the 12 January 2013 event at Stromboli, B. Volcanol., 78, 1–16,
<ext-link xlink:href="https://doi.org/10.1007/s00445-016-1033-4" ext-link-type="DOI">10.1007/s00445-016-1033-4</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><mixed-citation>
Capparelli, G. and Versace, P.: FLaIR and SUSHI: Two mathematical models for
early warning of landslides induced by rainfall, Landslides, 8, 67–79,
2011.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><mixed-citation>
Carlà, T., Intrieri, E., Di Traglia, F. and Casagli, N.: A
statistical-based approach for determining the intensity of unrest phases at
Stromboli volcano (Southern Italy) using one-step-ahead forecasts of
displacement time series, Nat. Hazards, 84, 669–683, 2016a.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><mixed-citation>
Carlà, T., Intrieri, E., Di Traglia, F., Nolesini, T., Gigli, G., and
Casagli, N.: Guidelines on the use of inverse velocity method as a tool for
setting alarm thresholds and forecasting landslides and structure collapses,
Landslides, 14, 517–534, 2016b.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><mixed-citation>Cascini, L., Fornaro, G., and Peduto, D.: Advanced low- and full-resolution
DInSAR map generation for slowmoving landslide analysis at different scales,
Eng. Geol., 112, 29–42, <ext-link xlink:href="https://doi.org/10.1016/j.enggeo.2010.01.003" ext-link-type="DOI">10.1016/j.enggeo.2010.01.003</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><mixed-citation>Cascini, L., Peduto, D., Pisciotta, G., Arena, L., Ferlisi, S., and Fornaro,
G.: The combination of DInSAR and facility damage data for the updating of
slow-moving landslide inventory maps at medium scale, Nat. Hazards Earth
Syst. Sci., 13, 1527–1549, <ext-link xlink:href="https://doi.org/10.5194/nhess-13-1527-2013" ext-link-type="DOI">10.5194/nhess-13-1527-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><mixed-citation>
Colesanti, C. and Wasowski, J.: Investigating landslides with space-borne
Synthetic Aperture Radar (SAR) interferometry, Eng. Geol., 88, 173–199,
2006.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><mixed-citation>
Costanzo, S., Di Massa, G., Costanzo, A., Morrone, L., Raffo, A., Spadafora,
F., Borgia, A., Formetta, G., Capparelli, G., and Versace, P.: Low-cost
radars integrated into a landslide early warning system, Adv. Intell. Syst.,
354, 11–19, 2015.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><mixed-citation>
Costanzo, S., Di Massa, G., Costanzo, A., Borgia, A., Raffo, A., Viggiani, G.
and Versace, P.: Software-defined radar system for landslides monitoring,
Adv. Intell. Syst., 445, 325–331, 2016.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><mixed-citation>
Crosta, G. B. and Agliardi, F.: How to obtain alert velocity thresholds for
large rockslides, Phys. Chem. Earth., Pt. A/B/C, 27, 1557–1565, 2002.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><mixed-citation>Del Ventisette, C., Intrieri, E., Luzi, G., Casagli, N., Fanti, R., and Leva,
D.: Using ground based radar interferometry during emergency: the case of the
A3 motorway (Calabria Region, Italy) threatened by a landslide, Nat. Hazards
Earth Syst. Sci., 11, 2483–2495, <ext-link xlink:href="https://doi.org/10.5194/nhess-11-2483-2011" ext-link-type="DOI">10.5194/nhess-11-2483-2011</ext-link>,
2011.</mixed-citation></ref>
      <ref id="bib1.bib19"><label>19</label><mixed-citation>
Di Traglia, F., Nolesini, T., Intrieri, E., Mugnai, F., Leva, D., Rosi, M.,
and Casagli N.: Review of ten years of volcano deformations recorded by the
ground-based InSAR monitoring system at Stromboli volcano: a tool to mitigate
volcano flank dynamics and intense volcanic activity, Earth-Sci. Rev., 139,
317–335, 2014.</mixed-citation></ref>
      <ref id="bib1.bib20"><label>20</label><mixed-citation>
Du, J., Yin, K., and Lacasse, S.: Displacement prediction in colluvial
landslides, three Gorges reservoir, China, Landslides, 10, 203–218, 2013.</mixed-citation></ref>
      <ref id="bib1.bib21"><label>21</label><mixed-citation>
Fei, X., Zheng, Q., Tang, T., Wang, Y., Wang, P., Liu, W., and Yang, H.: A
reliable transfer protocol for multi-parameter data collecting in wireless
sensor networks, 2013 15th Int Conf Adv Commun: Smart Services with Internet
of Things, ICACT 2013, 569–573, 2013.</mixed-citation></ref>
      <ref id="bib1.bib22"><label>22</label><mixed-citation>
Geertsema, M., Schwab, J. W., Blais-Stevens, A., and Sakals, M. E.:
Landslides impacting linear infrastructure in west central British Columbia,
Nat. Hazards, 48, 59–72, 2009.</mixed-citation></ref>
      <ref id="bib1.bib23"><label>23</label><mixed-citation>
Gene Corley, W., Mlakar, P. F. Sr., Sozen, M. A., and Thornton, C. H.: The
Oklahoma City bombing: Summary and recommendations for multihazard
mitigation, J. Perform. Constr. Fac., 12, 100–112, 1998.</mixed-citation></ref>
      <ref id="bib1.bib24"><label>24</label><mixed-citation>
Hadadian, H. and Kavian, Y.: Cross-layer protocol using contention mechanism
for supporting big data in wireless sensor network, 2016 10th International
Symposium on Communication Systems, Networks and Digital Signal Processing
(CSNDSP), 2016.</mixed-citation></ref>
      <ref id="bib1.bib25"><label>25</label><mixed-citation>
Intrieri, E., Gigli, G., Mugnai, F., Fanti, R., and Casagli, N.: Design and
implementation of a landslide early warning system, Eng. Geol., 147–148,
124–136, 2012.</mixed-citation></ref>
      <ref id="bib1.bib26"><label>26</label><mixed-citation>Intrieri, E., Gigli, G., Casagli, N., and Nadim, F.: Brief communication
“Landslide Early Warning System: toolbox and general concepts”, Nat.
Hazards Earth Syst. Sci., 13, 85–90,
<ext-link xlink:href="https://doi.org/10.5194/nhess-13-85-2013" ext-link-type="DOI">10.5194/nhess-13-85-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib27"><label>27</label><mixed-citation>
Intrieri, E., Gigli, G., Nocentini, M., Lombardi, L., Mugnai, F., and
Casagli, N.: Sinkhole monitoring and early warning: An experimental and
successful GB-InSAR application, Geomorphology, 241, 304–314, 2015.</mixed-citation></ref>
      <ref id="bib1.bib28"><label>28</label><mixed-citation>
Kadri, F., Birregah, B., and Châtelet, E.: The impact of natural
disasters on critical infrastructures: A domino effect-based study, J. Homel.
Secur. Emerg., 11, 217–241, 2014.</mixed-citation></ref>
      <ref id="bib1.bib29"><label>29</label><mixed-citation>
Khaday, B., Matson, E. T., Springer, J., Kwon, Y. K., Kim, H., Kim, S.,
Kenzhebalin, D., Sukyeong, C., Yoon, J., and Woo, H. S.: Wireless Sensor
Network and Big Data in Cooperative Fire Security system using HARMS, 2015
6th International Conference on Automation, Robotics and Applications
(ICARA), 2015.</mixed-citation></ref>
      <ref id="bib1.bib30"><label>30</label><mixed-citation>
Kim, Y., Bae, P., Han, J., and Ko, Y. B.: Data aggregation in precision
agriculture for low-power and lossy networks, 2015 IEEE Pacif, 2015.</mixed-citation></ref>
      <ref id="bib1.bib31"><label>31</label><mixed-citation>
Kröger, W.: Critical infrastructures at risk: A need for a new conceptual
approach and extended analytical tool, Reliab. Eng. Syst. Safe, 93,
1781–1787, 2008.</mixed-citation></ref>
      <ref id="bib1.bib32"><label>32</label><mixed-citation>
Labaka, L., Hernantes, J., and Sarriegi, J. M.: A holistic framework for
building critical infrastructure resilience, Technol. Forecast Soc., 103,
21–33, 2016.</mixed-citation></ref>
      <ref id="bib1.bib33"><label>33</label><mixed-citation>
Liu, H., Meng, Z., and Cui S.: A Wireless Sensor Network Prototype for
Environmental Monitoring in Greenhouses, 2007 Int C Wirel Comm Net, 2007.</mixed-citation></ref>
      <ref id="bib1.bib34"><label>34</label><mixed-citation>
Lombardi, L., Nocentini, M., Frodella, W., Nolesini, T., Bardi, F., Intrieri,
E., Carlà, T., Solari, L., Dotta, G., Ferrigno, F., and Casagli, N.: The
Calatabiano landslide (southern Italy): preliminary GB-InSAR monitoring data
and remote 3D mapping, Landslides, 14, 1–12,
2016.</mixed-citation></ref>
      <ref id="bib1.bib35"><label>35</label><mixed-citation>Luzi, G.: Ground Based SAR Interferometry: a novel tool for geoscience, in:
Geoscience and Remote Sensing. New Achievements, edited by: Imperatore, P.
and Riccio, D., InTech, available at:
<uri>http://www.intechopen.com/articles/show/title/ground-based-sar-interferometry-a-novel-tool-for-geoscience</uri>,
1–26, <ext-link xlink:href="https://doi.org/10.5772/9090" ext-link-type="DOI">10.5772/9090</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib36"><label>36</label><mixed-citation>Martino, S. and Mazzanti, P.: Integrating geomechanical surveys and remote
sensing for sea cliff slope stability analysis: the Mt. Pucci case study
(Italy), Nat. Hazards Earth Syst. Sci., 14, 831–848,
<ext-link xlink:href="https://doi.org/10.5194/nhess-14-831-2014" ext-link-type="DOI">10.5194/nhess-14-831-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib37"><label>37</label><mixed-citation>
Monserrat, O., Crosetto, M., and Luzi, G.: A review of ground-based SAR
interferometry for deformation measurement, ISPRS J. Photogramm, 93, 40–48,
2014.</mixed-citation></ref>
      <ref id="bib1.bib38"><label>38</label><mixed-citation>
Parthasarathy, A., Chaturvedi, A., Kokane, S., Warty, C., and Nema, S.:
Transmission of big data over MANETs, Aerosp Conf Proc, 2015.</mixed-citation></ref>
      <ref id="bib1.bib39"><label>39</label><mixed-citation>
Rudolf, H., Leva, D., Tarchi, D., and Sieber, A. J.: A mobile and versatile
SAR system, IGARSS Proc., Hamburh, 1999.</mixed-citation></ref>
      <ref id="bib1.bib40"><label>40</label><mixed-citation>Severin, J., Eberhardt, E., Leoni, L., and Fortin, S.: Development and
application of a pseudo-3D pit slope displacement map derived from
ground-based radar, Eng. Geol., 181, 202–211, 2014.
 </mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib41"><label>41</label><mixed-citation>
Sirangelo, B., Versace, P., and Capparelli, G.: Forewarning model for
landslides triggered by rainfall based on the analysis of historical data
file, IAHS-AISH P., 278, 298–304, 2003.</mixed-citation></ref>
      <ref id="bib1.bib42"><label>42</label><mixed-citation>
Snyder, L. and Burns, A. A.: Framework for critical infrastructure resilience
analysis. Energy and systems analysis-infrastructure, Sandia National
Laboratories, 2009.</mixed-citation></ref>
      <ref id="bib1.bib43"><label>43</label><mixed-citation>
Tapete, D., Casagli, N., Luzi, G., Fanti, R., Gigli, G., and Leva, D.:
Integrating radar and laser-based remote sensing techniques for monitoring
structural deformation of archaeological monuments, J. Archaeol. Sci., 40,
176–189, 2013.</mixed-citation></ref>
      <ref id="bib1.bib44"><label>44</label><mixed-citation>
Tarchi, D., Ohlmer, E., and Sieber, A. J.: Monitoring of structural changes
by radar interferometry, Res. Nondestruct. Eval., 9, 213–225, 1997.</mixed-citation></ref>
      <ref id="bib1.bib45"><label>45</label><mixed-citation>
Tarchi, D., Rudolf, H., Luzi, G., Chiarantini, L., Coppo, P., and Sieber, A.
J.: SAR interferometry for structural change detection: a demonstration test
on a dam, Int. Geosci. Remote Sens., 3, 1525–1527, 1999.</mixed-citation></ref>
      <ref id="bib1.bib46"><label>46</label><mixed-citation>
Tarchi, D., Casagli, N., Fanti, R., Leva, D., Luzi, G., Pasuto, A.,
Pieraccini, M., and Silvano, S.: Landslide monitoring by using ground-based
SAR interferometry: an example of application to the Tessina landslide in
Italy, Eng. Geol., 68, 15–30, 2003.</mixed-citation></ref>
      <ref id="bib1.bib47"><label>47</label><mixed-citation>
Urlainis, A., Shohet, I. M., Levy, R., Ornai, D., and Vilnay, O.: Damage in
critical infrastructures due to natural and man-made extreme Events – A
critical review, Procedia Engineer, 85, 529–535, 2014.</mixed-citation></ref>
      <ref id="bib1.bib48"><label>48</label><mixed-citation>
Urlainis, A., Shohet, I. M., and Levy, R.: Probabilistic Risk Assessment of
Oil and Gas Infrastructures for Seismic Extreme Events, Procedia Engineer,
123, 590–598, 2015.</mixed-citation></ref>
      <ref id="bib1.bib49"><label>49</label><mixed-citation>
Venkateswaran, V. and Kennedy, I.: How to sleep, control and transfer data in
an energy constrained wireless sensor network, 51st Annual Allerton
Conference on Communication, Control, and Computing (Allerton), 2013.</mixed-citation></ref>
      <ref id="bib1.bib50"><label>50</label><mixed-citation>
Versace, P., Capparelli, G., Leone, S., Artese, G., Costanzo, S., Corsonello,
P., Di Massa, G., Mendicino, G., Maletta, D., Muto, F., Senatore, A.,
Troncone, A., Conte, E., and Galletta, D.: LEWIS project: An integrated
system of monitoring, early warning and mitigation of landslides risk,
Rendiconti Online Società Geologica Italiana, 21, 586–587, 2012.</mixed-citation></ref>
      <ref id="bib1.bib51"><label>51</label><mixed-citation>
Yoo, S., Kim, J., Kim, T., Ahn, S., Sung, J. and Kim, D.: A2S: Automated
Agriculture System based on WSN, I Symp. Consum Electr., 2007.</mixed-citation></ref>

  </ref-list><app-group content-type="float"><app><title/>

    </app></app-group></back>
    <!--<article-title-html>Big data managing in a landslide early warning system: experience from a ground-based interferometric radar application</article-title-html>
<abstract-html><p class="p">A big challenge in terms or landslide risk mitigation is represented by
increasing the resiliency of society exposed to the risk. Among the
possible strategies with which to reach this goal, there is the implementation of
early warning systems. This paper describes a procedure to improve early warning
activities in areas affected by high landslide risk, such as those
classified as critical infrastructures for their central role in society.</p><p class="p">This research is part of the project <q>LEWIS (Landslides Early Warning
Integrated System): An Integrated System for Landslide Monitoring, Early
Warning and Risk Mitigation along Lifelines</q>.</p><p class="p">LEWIS is composed of a susceptibility assessment methodology providing
information for single points and areal monitoring systems, a data
transmission network and a data collecting and processing center (DCPC),
where readings from all monitoring systems and mathematical models converge
and which sets the basis for warning and intervention activities.</p><p class="p">The aim of this paper is to show how logistic issues linked to advanced
monitoring techniques, such as big data transfer and storing, can be dealt
with compatibly with an early warning system. Therefore, we focus on the
interaction between an areal monitoring tool (a ground-based interferometric
radar) and the DCPC. By converting complex data into ASCII strings and
through appropriate data cropping and average, and by implementing an
algorithm for line-of-sight correction, we managed to reduce the data daily
output without compromising the capability for performing.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
Antonello, G., Casagli, N., Farina, P., Leva, D., Nico, G., Sieber, A. J.,
and Tarchi, D.: Ground-based SAR interferometry for monitoring mass
movements, Landslides, 1, 21–28, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
Baldridge, S. M. and Marshall, J. D.: Performance of structures in the January
2010 MW 7.0 Haiti earthquake, Structures Congress, 1660–1671, <a href="https://doi.org/10.1061/41171(401)145" target="_blank">https://doi.org/10.1061/41171(401)145</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
Bamler, R. and Hartl, P.: Synthetic Aperture Radar Interferometry, Inverse
Probl., 14, R1–R54, 1998.
</mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
Bardi, F., Frodella, W., Ciampalini, A., Del Ventisette, C., Gigli, G.,
Fanti, R., Basile, G., Moretti, S., and Casagli, N.: Integration between
ground based and satellite SAR data in landslide mapping: The San Fratello
case study, Geomorphology, 223, 45–60, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
Bardi, F., Raspini, F., Ciampalini, A., Kristensen, L., Rouyet, L., Lauknes,
T. R., Frauenfelder, R., and Casagli, N.: Space-Borne and Ground-Based InSAR
Data Integration: The Åknes Test Site, Remote Sens.-Basel., 8, 237, <a href="https://doi.org/10.3390/rs8030237" target="_blank">https://doi.org/10.3390/rs8030237</a>,
2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
Bardi, F., Raspini, F., Frodella, W., Lombardi, L., Nocentini, M., Gigli,
G., Morelli, S., Corsini, A., and Casagli, N.: Monitoring the Rapid-Moving
reactivation of Earth Flows by Means of GB-InSAR: The April 2013 Capriglio
Landslide (Northern Appennines, Italy),
Remote Sens.-Basel., 9, 165, <a href="https://doi.org/10.3390/rs9020165" target="_blank">https://doi.org/10.3390/rs9020165</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
Cagno, E., De Ambroggi, M., Grande, O., and Trucco, T.: Risk analysis of
underground infrastructures in urban areas, Reliab. Eng. Syst. Safe, 96,
139–148, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
Calvari, S., Intrieri, E., Di Traglia, F., Bonaccorso, A., Casagli, N., and
Cristaldi, A.: Monitoring crater-wall collapse at active volcanoes: a study
of the 12 January 2013 event at Stromboli, B. Volcanol., 78, 1–16,
<a href="https://doi.org/10.1007/s00445-016-1033-4" target="_blank">https://doi.org/10.1007/s00445-016-1033-4</a>, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation>
Capparelli, G. and Versace, P.: FLaIR and SUSHI: Two mathematical models for
early warning of landslides induced by rainfall, Landslides, 8, 67–79,
2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
Carlà, T., Intrieri, E., Di Traglia, F. and Casagli, N.: A
statistical-based approach for determining the intensity of unrest phases at
Stromboli volcano (Southern Italy) using one-step-ahead forecasts of
displacement time series, Nat. Hazards, 84, 669–683, 2016a.
</mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
Carlà, T., Intrieri, E., Di Traglia, F., Nolesini, T., Gigli, G., and
Casagli, N.: Guidelines on the use of inverse velocity method as a tool for
setting alarm thresholds and forecasting landslides and structure collapses,
Landslides, 14, 517–534, 2016b.
</mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
Cascini, L., Fornaro, G., and Peduto, D.: Advanced low- and full-resolution
DInSAR map generation for slowmoving landslide analysis at different scales,
Eng. Geol., 112, 29–42, <a href="https://doi.org/10.1016/j.enggeo.2010.01.003" target="_blank">https://doi.org/10.1016/j.enggeo.2010.01.003</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
Cascini, L., Peduto, D., Pisciotta, G., Arena, L., Ferlisi, S., and Fornaro,
G.: The combination of DInSAR and facility damage data for the updating of
slow-moving landslide inventory maps at medium scale, Nat. Hazards Earth
Syst. Sci., 13, 1527–1549, <a href="https://doi.org/10.5194/nhess-13-1527-2013" target="_blank">https://doi.org/10.5194/nhess-13-1527-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
Colesanti, C. and Wasowski, J.: Investigating landslides with space-borne
Synthetic Aperture Radar (SAR) interferometry, Eng. Geol., 88, 173–199,
2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation>
Costanzo, S., Di Massa, G., Costanzo, A., Morrone, L., Raffo, A., Spadafora,
F., Borgia, A., Formetta, G., Capparelli, G., and Versace, P.: Low-cost
radars integrated into a landslide early warning system, Adv. Intell. Syst.,
354, 11–19, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation>
Costanzo, S., Di Massa, G., Costanzo, A., Borgia, A., Raffo, A., Viggiani, G.
and Versace, P.: Software-defined radar system for landslides monitoring,
Adv. Intell. Syst., 445, 325–331, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation>
Crosta, G. B. and Agliardi, F.: How to obtain alert velocity thresholds for
large rockslides, Phys. Chem. Earth., Pt. A/B/C, 27, 1557–1565, 2002.
</mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
Del Ventisette, C., Intrieri, E., Luzi, G., Casagli, N., Fanti, R., and Leva,
D.: Using ground based radar interferometry during emergency: the case of the
A3 motorway (Calabria Region, Italy) threatened by a landslide, Nat. Hazards
Earth Syst. Sci., 11, 2483–2495, <a href="https://doi.org/10.5194/nhess-11-2483-2011" target="_blank">https://doi.org/10.5194/nhess-11-2483-2011</a>,
2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
Di Traglia, F., Nolesini, T., Intrieri, E., Mugnai, F., Leva, D., Rosi, M.,
and Casagli N.: Review of ten years of volcano deformations recorded by the
ground-based InSAR monitoring system at Stromboli volcano: a tool to mitigate
volcano flank dynamics and intense volcanic activity, Earth-Sci. Rev., 139,
317–335, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation>
Du, J., Yin, K., and Lacasse, S.: Displacement prediction in colluvial
landslides, three Gorges reservoir, China, Landslides, 10, 203–218, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib21"><label>21</label><mixed-citation>
Fei, X., Zheng, Q., Tang, T., Wang, Y., Wang, P., Liu, W., and Yang, H.: A
reliable transfer protocol for multi-parameter data collecting in wireless
sensor networks, 2013 15th Int Conf Adv Commun: Smart Services with Internet
of Things, ICACT 2013, 569–573, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib22"><label>22</label><mixed-citation>
Geertsema, M., Schwab, J. W., Blais-Stevens, A., and Sakals, M. E.:
Landslides impacting linear infrastructure in west central British Columbia,
Nat. Hazards, 48, 59–72, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib23"><label>23</label><mixed-citation>
Gene Corley, W., Mlakar, P. F. Sr., Sozen, M. A., and Thornton, C. H.: The
Oklahoma City bombing: Summary and recommendations for multihazard
mitigation, J. Perform. Constr. Fac., 12, 100–112, 1998.
</mixed-citation></ref-html>
<ref-html id="bib1.bib24"><label>24</label><mixed-citation>
Hadadian, H. and Kavian, Y.: Cross-layer protocol using contention mechanism
for supporting big data in wireless sensor network, 2016 10th International
Symposium on Communication Systems, Networks and Digital Signal Processing
(CSNDSP), 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib25"><label>25</label><mixed-citation>
Intrieri, E., Gigli, G., Mugnai, F., Fanti, R., and Casagli, N.: Design and
implementation of a landslide early warning system, Eng. Geol., 147–148,
124–136, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib26"><label>26</label><mixed-citation>
Intrieri, E., Gigli, G., Casagli, N., and Nadim, F.: Brief communication
“Landslide Early Warning System: toolbox and general concepts”, Nat.
Hazards Earth Syst. Sci., 13, 85–90,
<a href="https://doi.org/10.5194/nhess-13-85-2013" target="_blank">https://doi.org/10.5194/nhess-13-85-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>27</label><mixed-citation>
Intrieri, E., Gigli, G., Nocentini, M., Lombardi, L., Mugnai, F., and
Casagli, N.: Sinkhole monitoring and early warning: An experimental and
successful GB-InSAR application, Geomorphology, 241, 304–314, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>28</label><mixed-citation>
Kadri, F., Birregah, B., and Châtelet, E.: The impact of natural
disasters on critical infrastructures: A domino effect-based study, J. Homel.
Secur. Emerg., 11, 217–241, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib29"><label>29</label><mixed-citation>
Khaday, B., Matson, E. T., Springer, J., Kwon, Y. K., Kim, H., Kim, S.,
Kenzhebalin, D., Sukyeong, C., Yoon, J., and Woo, H. S.: Wireless Sensor
Network and Big Data in Cooperative Fire Security system using HARMS, 2015
6th International Conference on Automation, Robotics and Applications
(ICARA), 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation>
Kim, Y., Bae, P., Han, J., and Ko, Y. B.: Data aggregation in precision
agriculture for low-power and lossy networks, 2015 IEEE Pacif, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation>
Kröger, W.: Critical infrastructures at risk: A need for a new conceptual
approach and extended analytical tool, Reliab. Eng. Syst. Safe, 93,
1781–1787, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib32"><label>32</label><mixed-citation>
Labaka, L., Hernantes, J., and Sarriegi, J. M.: A holistic framework for
building critical infrastructure resilience, Technol. Forecast Soc., 103,
21–33, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib33"><label>33</label><mixed-citation>
Liu, H., Meng, Z., and Cui S.: A Wireless Sensor Network Prototype for
Environmental Monitoring in Greenhouses, 2007 Int C Wirel Comm Net, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation>
Lombardi, L., Nocentini, M., Frodella, W., Nolesini, T., Bardi, F., Intrieri,
E., Carlà, T., Solari, L., Dotta, G., Ferrigno, F., and Casagli, N.: The
Calatabiano landslide (southern Italy): preliminary GB-InSAR monitoring data
and remote 3D mapping, Landslides, 14, 1–12,
2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation>
Luzi, G.: Ground Based SAR Interferometry: a novel tool for geoscience, in:
Geoscience and Remote Sensing. New Achievements, edited by: Imperatore, P.
and Riccio, D., InTech, available at:
<a href="http://www.intechopen.com/articles/show/title/ground-based-sar-interferometry-a-novel-tool-for-geoscience" target="_blank">http://www.intechopen.com/articles/show/title/ground-based-sar-interferometry-a-novel-tool-for-geoscience</a>,
1–26, <a href="https://doi.org/10.5772/9090" target="_blank">https://doi.org/10.5772/9090</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib36"><label>36</label><mixed-citation>
Martino, S. and Mazzanti, P.: Integrating geomechanical surveys and remote
sensing for sea cliff slope stability analysis: the Mt. Pucci case study
(Italy), Nat. Hazards Earth Syst. Sci., 14, 831–848,
<a href="https://doi.org/10.5194/nhess-14-831-2014" target="_blank">https://doi.org/10.5194/nhess-14-831-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib37"><label>37</label><mixed-citation>
Monserrat, O., Crosetto, M., and Luzi, G.: A review of ground-based SAR
interferometry for deformation measurement, ISPRS J. Photogramm, 93, 40–48,
2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib38"><label>38</label><mixed-citation>
Parthasarathy, A., Chaturvedi, A., Kokane, S., Warty, C., and Nema, S.:
Transmission of big data over MANETs, Aerosp Conf Proc, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib39"><label>39</label><mixed-citation>
Rudolf, H., Leva, D., Tarchi, D., and Sieber, A. J.: A mobile and versatile
SAR system, IGARSS Proc., Hamburh, 1999.
</mixed-citation></ref-html>
<ref-html id="bib1.bib40"><label>40</label><mixed-citation>
Severin, J., Eberhardt, E., Leoni, L., and Fortin, S.: Development and
application of a pseudo-3D pit slope displacement map derived from
ground-based radar, Eng. Geol., 181, 202–211, 2014.

</mixed-citation></ref-html>
<ref-html id="bib1.bib41"><label>41</label><mixed-citation>
Sirangelo, B., Versace, P., and Capparelli, G.: Forewarning model for
landslides triggered by rainfall based on the analysis of historical data
file, IAHS-AISH P., 278, 298–304, 2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib42"><label>42</label><mixed-citation>
Snyder, L. and Burns, A. A.: Framework for critical infrastructure resilience
analysis. Energy and systems analysis-infrastructure, Sandia National
Laboratories, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib43"><label>43</label><mixed-citation>
Tapete, D., Casagli, N., Luzi, G., Fanti, R., Gigli, G., and Leva, D.:
Integrating radar and laser-based remote sensing techniques for monitoring
structural deformation of archaeological monuments, J. Archaeol. Sci., 40,
176–189, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib44"><label>44</label><mixed-citation>
Tarchi, D., Ohlmer, E., and Sieber, A. J.: Monitoring of structural changes
by radar interferometry, Res. Nondestruct. Eval., 9, 213–225, 1997.
</mixed-citation></ref-html>
<ref-html id="bib1.bib45"><label>45</label><mixed-citation>
Tarchi, D., Rudolf, H., Luzi, G., Chiarantini, L., Coppo, P., and Sieber, A.
J.: SAR interferometry for structural change detection: a demonstration test
on a dam, Int. Geosci. Remote Sens., 3, 1525–1527, 1999.
</mixed-citation></ref-html>
<ref-html id="bib1.bib46"><label>46</label><mixed-citation>
Tarchi, D., Casagli, N., Fanti, R., Leva, D., Luzi, G., Pasuto, A.,
Pieraccini, M., and Silvano, S.: Landslide monitoring by using ground-based
SAR interferometry: an example of application to the Tessina landslide in
Italy, Eng. Geol., 68, 15–30, 2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib47"><label>47</label><mixed-citation>
Urlainis, A., Shohet, I. M., Levy, R., Ornai, D., and Vilnay, O.: Damage in
critical infrastructures due to natural and man-made extreme Events – A
critical review, Procedia Engineer, 85, 529–535, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib48"><label>48</label><mixed-citation>
Urlainis, A., Shohet, I. M., and Levy, R.: Probabilistic Risk Assessment of
Oil and Gas Infrastructures for Seismic Extreme Events, Procedia Engineer,
123, 590–598, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib49"><label>49</label><mixed-citation>
Venkateswaran, V. and Kennedy, I.: How to sleep, control and transfer data in
an energy constrained wireless sensor network, 51st Annual Allerton
Conference on Communication, Control, and Computing (Allerton), 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib50"><label>50</label><mixed-citation>
Versace, P., Capparelli, G., Leone, S., Artese, G., Costanzo, S., Corsonello,
P., Di Massa, G., Mendicino, G., Maletta, D., Muto, F., Senatore, A.,
Troncone, A., Conte, E., and Galletta, D.: LEWIS project: An integrated
system of monitoring, early warning and mitigation of landslides risk,
Rendiconti Online Società Geologica Italiana, 21, 586–587, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib51"><label>51</label><mixed-citation>
Yoo, S., Kim, J., Kim, T., Ahn, S., Sung, J. and Kim, D.: A2S: Automated
Agriculture System based on WSN, I Symp. Consum Electr., 2007.
</mixed-citation></ref-html>--></article>
