Articles | Volume 22, issue 12
https://doi.org/10.5194/nhess-22-3839-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/nhess-22-3839-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
30 Nov 2022
Research article |
| 30 Nov 2022
| 30 Nov 2022
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands)
María Teresa Pedrosa-González
Departamento de Geodinámica, Universidad de Granada, 18071
Granada, Spain
José Manuel González-Vida
Departamento de Matemática Aplicada, Escuela de Ingenierías
Industriales, Universidad de Málaga, 29071 Málaga, Spain
Jesús Galindo-Záldivar
Departamento de Geodinámica, Universidad de Granada, 18071
Granada, Spain
Departamento de Geociencias Marinas, Instituto Andaluz de Ciencias de la Tierra, Consejo Superior de Investigaciones Científicas y Universidad de Granada (CSIC-UGR), 18100 Granada, Spain
Sergio Ortega
Departamento de Matemática Aplicada, Escuela de Ingenierías
Industriales, Universidad de Málaga, 29071 Málaga, Spain
Manuel Jesús Castro
Departamento de Análisis Matemático, Estadística e Investigación Operativa, y Matemática Aplicada, Facultad de Ciencias, Universidad de Málaga, 29071 Málaga, Spain
David Casas
Marine Geosciences, Institut de Ciències del Mar (ICM), Consejo Superior de Investigaciones Cientificas (CSIC), 08003 Barcelona, Spain
Gemma Ercilla
CORRESPONDING AUTHOR
Marine Geosciences, Institut de Ciències del Mar (ICM), Consejo Superior de Investigaciones Cientificas (CSIC), 08003 Barcelona, Spain
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Alice Abbate, José M. González Vida, Manuel J. Castro Díaz, Fabrizio Romano, Hafize Başak Bayraktar, Andrey Babeyko, and Stefano Lorito
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-41, https://doi.org/10.5194/nhess-2024-41, 2024
Preprint under review for NHESS
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Modeling the tsunami generation due to a rapid submarine earthquake is a complex problem. We propose and test, under a variety of realistic conditions in a subduction zone, an efficient solution to this problem, and a tool which can compute the generation of any potential tsunami in any ocean of the world. We will explore in the future solutions which would allow us to model the tsunami generation also by slower (time-dependent) seafloor displacement.
Manfred Lafosse, Elia d'Acremont, Alain Rabaute, Ferran Estrada, Martin Jollivet-Castelot, Juan Tomas Vazquez, Jesus Galindo-Zaldivar, Gemma Ercilla, Belen Alonso, Jeroen Smit, Abdellah Ammar, and Christian Gorini
Solid Earth, 11, 741–765, https://doi.org/10.5194/se-11-741-2020, https://doi.org/10.5194/se-11-741-2020, 2020
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The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
José Manuel González-Vida, Jorge Macías, Manuel Jesús Castro, Carlos Sánchez-Linares, Marc de la Asunción, Sergio Ortega-Acosta, and Diego Arcas
Nat. Hazards Earth Syst. Sci., 19, 369–388, https://doi.org/10.5194/nhess-19-369-2019, https://doi.org/10.5194/nhess-19-369-2019, 2019
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In 1958, at Lituya Bay in Alaska, the largest tsunami wave ever recorded took place. Since then, its numerical simulation has been a challenge and no numerical model has been able to reproduce, in the real geometry of the bay, the more than 200 m wave and the extreme run-up (climbing of the water up on land) of 524 m. The aim of our research, in the framework of a collaboration between the University of Malága (Spain) and NOAA (US), was to fulfil this gap at the same time as verifying our model.
Irene Molinari, Roberto Tonini, Stefano Lorito, Alessio Piatanesi, Fabrizio Romano, Daniele Melini, Andreas Hoechner, José M. Gonzàlez Vida, Jorge Maciás, Manuel J. Castro, and Marc de la Asunción
Nat. Hazards Earth Syst. Sci., 16, 2593–2602, https://doi.org/10.5194/nhess-16-2593-2016, https://doi.org/10.5194/nhess-16-2593-2016, 2016
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We present a database of pre-calculated tsunami waveforms for the entire Mediterranean Sea, obtained by numerical propagation of uniformly spaced Gaussian-shaped elementary sources for the sea level elevation. Based on any initial sea surface displacement, the database allows the fast calculation of full waveforms of coastal sites. The resulting product is suitable for different applications such as probabilistic tsunami hazard, tsunami source inversions and tsunami warning systems.
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Nearshore tsunami amplitudes across the Maldives archipelago due to worst-case seismic scenarios in the Indian Ocean
Evidence of Middle Holocene landslide-generated tsunamis recorded in lake sediments from Saqqaq, West Greenland
Investigation of historical severe storms and storm tides in the German Bight with century reanalysis data
Proposal for a new meteotsunami intensity index
Total water levels along the South Atlantic Bight during three along-shelf propagating tropical cyclones: relative contributions of storm surge and wave runup
Hurricane Irma: an unprecedented event over the last 3700 years? Geomorphological changes and sedimentological record in Codrington Lagoon, Barbuda
Bayesian extreme value analysis of extreme sea levels along the German Baltic coast using historical information
Storm characteristics influence nitrogen removal in an urban estuarine environment
A new European coastal flood database for low–medium intensity events
Boulder transport and wave height of a seventeenth-century South China Sea tsunami on Penghu Islands, Taiwan
A wave-resolving modeling study of rip current variability, rip hazard, and swimmer escape strategies on an embayed beach
Human displacements from Tropical Cyclone Idai attributable to climate change
Influence of data source and copula statistics on estimates of compound extreme water levels in a river mouth environment
Three decades of coastal subsidence in the slow-moving Nice Côte d'Azur Airport area (France) revealed by InSAR (interferometric synthetic-aperture radar): insights into the deformation mechanism
Modelling extreme water levels using intertidal topography and bathymetry derived from multispectral satellite images
Regional assessment of extreme sea levels and associated coastal flooding along the German Baltic Sea coast
A systemic and comprehensive assessment of coastal hazard changes: method and application to France and its overseas territories
Joint probability analysis of storm surges and waves caused by tropical cyclones for the estimation of protection standard: a case study on the eastern coast of the Leizhou Peninsula and the island of Hainan in China
Meteotsunami in the United Kingdom: the hidden hazard
Climate-induced storminess forces major increases in future storm surge hazard in the South China Sea region
Assessing Typhoon Soulik-induced morphodynamics over the Mokpo coastal region in South Korea based on a geospatial approach
Bayesian hierarchical modelling of sea-level extremes in the Finnish coastal region
Simulating sea level extremes from synthetic low-pressure systems
Nonlinear processes in tsunami simulations for the Peruvian coast with focus on Lima/Callao
Assessing the coastal hazard of Medicane Ianos through ensemble modelling
A predictive equation for wave setup using genetic programming
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Compound flood events: analysing the joint occurrence of extreme river discharge events and storm surges in northern and central Europe
Improvements to the detection and analysis of external surges in the North Sea
Optimal probabilistic placement of facilities using a surrogate model for 3D tsunami simulations
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The role of preconditioning for extreme storm surges in the western Baltic Sea
Freak wave events in 2005–2021: statistics and analysis of favourable wave and wind conditions
Probabilistic projections and past trends of sea level rise in Finland
The effect of deep ocean currents on ocean- bottom seismometers records
An interdisciplinary agent-based evacuation model: integrating the natural environment, built environment, and social system for community preparedness and resilience
Coastal extreme sea levels in the Caribbean Sea induced by tropical cyclones
Characteristics of consecutive tsunamis and resulting tsunami behaviors in southern Taiwan induced by the Hengchun earthquake doublet on 26 December 2006
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Eric Mortensen, Timothy Tiggeloven, Toon Haer, Bas van Bemmel, Dewi Le Bars, Sanne Muis, Dirk Eilander, Frederiek Sperna Weiland, Arno Bouwman, Willem Ligtvoet, and Philip J. Ward
Nat. Hazards Earth Syst. Sci., 24, 1381–1400, https://doi.org/10.5194/nhess-24-1381-2024, https://doi.org/10.5194/nhess-24-1381-2024, 2024
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Current levels of coastal flood risk are projected to increase in coming decades due to various reasons, e.g. sea-level rise, land subsidence, and coastal urbanization: action is needed to minimize this future risk. We evaluate dykes and coastal levees, foreshore vegetation, zoning restrictions, and dry-proofing on a global scale to estimate what levels of risk reductions are possible. We demonstrate that there are several potential adaptation pathways forward for certain areas of the world.
Charlotte Lyddon, Nguyen Chien, Grigorios Vasilopoulos, Michael Ridgill, Sogol Moradian, Agnieszka Olbert, Thomas Coulthard, Andrew Barkwith, and Peter Robins
Nat. Hazards Earth Syst. Sci., 24, 973–997, https://doi.org/10.5194/nhess-24-973-2024, https://doi.org/10.5194/nhess-24-973-2024, 2024
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Recent storms in the UK, like Storm Ciara in 2020, show how vulnerable estuaries are to the combined effect of sea level and river discharge. We show the combinations of sea levels and river discharges that cause flooding in the Conwy estuary, N Wales. The results showed flooding was amplified under moderate conditions in the middle estuary and elsewhere sea state or river flow dominated the hazard. Combined sea and river thresholds can improve prediction and early warning of compound flooding.
Shuaib Rasheed, Simon C. Warder, Yves Plancherel, and Matthew D. Piggott
Nat. Hazards Earth Syst. Sci., 24, 737–755, https://doi.org/10.5194/nhess-24-737-2024, https://doi.org/10.5194/nhess-24-737-2024, 2024
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Here we use a high-resolution bathymetry dataset of the Maldives archipelago, as well as corresponding high numerical model resolution, to carry out a scenario-based tsunami hazard assessment for the entire Maldives archipelago to investigate the potential impact of plausible far-field tsunamis across the Indian Ocean at the island scale. The results indicate that several factors contribute to mitigating and amplifying tsunami waves at the island scale.
Niels J. Korsgaard, Kristian Svennevig, Anne S. Søndergaard, Gregor Luetzenburg, Mimmi Oksman, and Nicolaj K. Larsen
Nat. Hazards Earth Syst. Sci., 24, 757–772, https://doi.org/10.5194/nhess-24-757-2024, https://doi.org/10.5194/nhess-24-757-2024, 2024
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A tsunami wave will leave evidence of erosion and deposition in coastal lakes, making it possible to determine the runup height and when it occurred. Here, we use four lakes now located at elevations of 19–91 m a.s.l. close to the settlement of Saqqaq, West Greenland, to show that at least two giant tsunamis occurred 7300–7600 years ago with runup heights larger than 40 m. We infer that any tsunamis from at least nine giga-scale landslides must have happened 8500–10 000 years ago.
Elke Magda Inge Meyer and Lidia Gaslikova
Nat. Hazards Earth Syst. Sci., 24, 481–499, https://doi.org/10.5194/nhess-24-481-2024, https://doi.org/10.5194/nhess-24-481-2024, 2024
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Storm tides for eight extreme historical storms in the German Bight are modelled using sets of slightly varying atmospheric conditions from the century reanalyses. Comparisons with the water level observations from the gauges Norderney, Cuxhaven and Husum show that single members of the reanalyses are suitable for the reconstruction of extreme storms. Storms with more northerly tracks show less variability within a set and have more potential for accurate reconstruction of extreme water levels.
Clare Lewis, Tim Smyth, Jess Neumann, and Hannah Cloke
Nat. Hazards Earth Syst. Sci., 24, 121–131, https://doi.org/10.5194/nhess-24-121-2024, https://doi.org/10.5194/nhess-24-121-2024, 2024
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Meteotsunami are the result of atmospheric disturbances and can impact coastlines causing injury, loss of life, and damage to assets. This paper introduces a novel intensity index to allow for the quantification of these events at the shoreline. This has the potential to assist in the field of natural hazard assessment. It was trialled in the UK but designed for global applicability and to become a widely accepted standard in coastal planning, meteotsunami forecasting, and early warning systems.
Chu-En Hsu, Katherine A. Serafin, Xiao Yu, Christie A. Hegermiller, John C. Warner, and Maitane Olabarrieta
Nat. Hazards Earth Syst. Sci., 23, 3895–3912, https://doi.org/10.5194/nhess-23-3895-2023, https://doi.org/10.5194/nhess-23-3895-2023, 2023
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Total water levels (TWLs) induced by tropical cyclones (TCs) are among the leading hazards faced by coastal communities. Using numerical models, we examined how TWL components (surge and wave runup) along the South Atlantic Bight varied during hurricanes Matthew (2016), Dorian (2019), and Isaias (2020). Peak surge and peak wave runup were dominated by wind speeds and relative positions to TCs. The exceedance time of TWLs was controlled by normalized distances to TC and TC translation speeds.
Maude Biguenet, Eric Chaumillon, Pierre Sabatier, Antoine Bastien, Emeline Geba, Fabien Arnaud, Thibault Coulombier, and Nathalie Feuillet
Nat. Hazards Earth Syst. Sci., 23, 3761–3788, https://doi.org/10.5194/nhess-23-3761-2023, https://doi.org/10.5194/nhess-23-3761-2023, 2023
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This work documents the impact of Hurricane Irma (2017) on the Codrington barrier and lagoon on Barbuda Island. Irma caused two wide breaches in the sandy barrier, which remained unopened for 250 years. The thick and extensive sand sheet at the top of the lagoon fill was attributed to Irma. This unique deposit in a 3700-year record confirms Irma's exceptional character. This case study illustrates the consequences of high-intensity hurricanes in low-lying islands in a global warming context.
Leigh Richard MacPherson, Arne Arns, Svenja Fischer, Fernando Javier Méndez, and Jürgen Jensen
Nat. Hazards Earth Syst. Sci., 23, 3685–3701, https://doi.org/10.5194/nhess-23-3685-2023, https://doi.org/10.5194/nhess-23-3685-2023, 2023
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Efficient adaptation planning for coastal flooding caused by extreme sea levels requires accurate assessments of the underlying hazard. Tide-gauge data alone are often insufficient for providing the desired accuracy but may be supplemented with historical information. We estimate extreme sea levels along the German Baltic coast and show that relying solely on tide-gauge data leads to underestimations. Incorporating historical information leads to improved estimates with reduced uncertainties.
Anne Margaret H. Smiley, Suzanne P. Thompson, Nathan S. Hall, and Michael F. Piehler
Nat. Hazards Earth Syst. Sci., 23, 3635–3649, https://doi.org/10.5194/nhess-23-3635-2023, https://doi.org/10.5194/nhess-23-3635-2023, 2023
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Floodwaters can deliver reactive nitrogen to sensitive aquatic systems and diminish water quality. We assessed the nitrogen removal capabilities of flooded habitats and urban landscapes. Differences in processing rates across land cover treatments and between nutrient treatments suggest that abundance and spatial distributions of habitats, as well as storm characteristics, influence landscape-scale nitrogen removal. Results have important implications for coastal development and climate change.
Marine Le Gal, Tomás Fernández-Montblanc, Enrico Duo, Juan Montes Perez, Paulo Cabrita, Paola Souto Ceccon, Véra Gastal, Paolo Ciavola, and Clara Armaroli
Nat. Hazards Earth Syst. Sci., 23, 3585–3602, https://doi.org/10.5194/nhess-23-3585-2023, https://doi.org/10.5194/nhess-23-3585-2023, 2023
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Assessing coastal hazards is crucial to mitigate flooding disasters. In this regard, coastal flood databases are valuable tools. This paper describes a new coastal flood map catalogue covering the entire European coastline, as well as the methodology to build it and its accuracy. The catalogue focuses on frequent extreme events and relies on synthetic scenarios estimated from local storm conditions. Flood-prone areas and regions sensitive to storm duration and water level peak were identified.
Neng-Ti Yu, Cheng-Hao Lu, I-Chin Yen, Jia-Hong Chen, Jiun-Yee Yen, and Shyh-Jeng Chyi
Nat. Hazards Earth Syst. Sci., 23, 3525–3542, https://doi.org/10.5194/nhess-23-3525-2023, https://doi.org/10.5194/nhess-23-3525-2023, 2023
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A paleotsunami deposit of cliff-top basalt debris was identified on the Penghu Islands in the southern Taiwan Strait and related to the 1661 earthquake in southwest Taiwan. A minimum wave height of 3.2 m is estimated to have rotated the biggest boulder for over 30 m landwards onto the cliff top at 2.5 m a.s.l. The event must have been huge compared to the 1994 M 6.4 earthquake with the ensuing 0.4 m high tsunami in the same area, validating the intimidating tsunami risks in the South China Sea.
Ye Yuan, Huaiwei Yang, Fujiang Yu, Yi Gao, Benxia Li, and Chuang Xing
Nat. Hazards Earth Syst. Sci., 23, 3487–3507, https://doi.org/10.5194/nhess-23-3487-2023, https://doi.org/10.5194/nhess-23-3487-2023, 2023
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Rip currents are narrow jets of offshore-directed flow that originated in the surf zone, which can take swimmers of all ability levels into deeper water unawares. In this study, a 1 m fine-resolution wave-resolving model was configured to study rip current variability and the optimal swimmer escape strategies. Multiple factors contribute to the survival of swimmers. However, for weak-to-moderate rip and longshore currents, swimming onshore consistently seems to be the most successful strategy.
Benedikt Mester, Thomas Vogt, Seth Bryant, Christian Otto, Katja Frieler, and Jacob Schewe
Nat. Hazards Earth Syst. Sci., 23, 3467–3485, https://doi.org/10.5194/nhess-23-3467-2023, https://doi.org/10.5194/nhess-23-3467-2023, 2023
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In 2019, Cyclone Idai displaced more than 478 000 people in Mozambique. In our study, we use coastal flood modeling and satellite imagery to construct a counterfactual cyclone event without the effects of climate change. We show that 12 600–14 900 displacements can be attributed to sea level rise and the intensification of storm wind speeds due to global warming. Our impact attribution study is the first one on human displacement and one of very few for a low-income country.
Kévin Dubois, Morten Andreas Dahl Larsen, Martin Drews, Erik Nilsson, and Anna Rutgersson
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-176, https://doi.org/10.5194/nhess-2023-176, 2023
Revised manuscript under review for NHESS
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Both extreme river discharge and storm surges can interact at the coast and lead to flooding. However, it is difficult to predict flood levels during such compound events because they are rare and complex. Here, we focus on the quantification of uncertainties; and we investigate the sources of limitations while carrying out such analyses at Halmstad city (Sweden). Based on a sensitivity analysis, we emphasize that both the choice of data source and statistical methodology influence the results.
Olivier Cavalié, Frédéric Cappa, and Béatrice Pinel-Puysségur
Nat. Hazards Earth Syst. Sci., 23, 3235–3246, https://doi.org/10.5194/nhess-23-3235-2023, https://doi.org/10.5194/nhess-23-3235-2023, 2023
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Coastal areas are fragile ecosystems that face multiple hazards. In this study, we measured the downward motion of the Nice Côte d'Azur Airport (France) that was built on reclaimed area and found that it has subsided from 16 mm yr-1 in the 1990s to 8 mm yr-1 today. A continuous remote monitoring of the platform will provide key data for a detailed investigation of future subsidence maps, and this contribution will help to evaluate the potential failure of part of the airport platform.
Wagner L. L. Costa, Karin R. Bryan, and Giovanni Coco
Nat. Hazards Earth Syst. Sci., 23, 3125–3146, https://doi.org/10.5194/nhess-23-3125-2023, https://doi.org/10.5194/nhess-23-3125-2023, 2023
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For predicting flooding events at the coast, topo-bathymetric data are essential. However, elevation data can be unavailable. To tackle this issue, recent efforts have centred on the use of satellite-derived topography (SDT) and bathymetry (SDB). This work is aimed at evaluating their accuracy and use for flooding prediction in enclosed estuaries. Results show that the use of SDT and SDB in numerical modelling can produce similar predictions when compared to the surveyed elevation data.
Joshua Kiesel, Marvin Lorenz, Marcel König, Ulf Gräwe, and Athanasios T. Vafeidis
Nat. Hazards Earth Syst. Sci., 23, 2961–2985, https://doi.org/10.5194/nhess-23-2961-2023, https://doi.org/10.5194/nhess-23-2961-2023, 2023
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Among the Baltic Sea littoral states, Germany is anticipated to experience considerable damage as a result of increased coastal flooding due to sea-level rise (SLR). Here we apply a new modelling framework to simulate how flooding along the German Baltic Sea coast may change until 2100 if dikes are not upgraded. We find that the study region is highly exposed to flooding, and we emphasise the importance of current plans to update coastal protection in the future.
Marc Igigabel, Marissa Yates, Michalis Vousdoukas, and Youssef Diab
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-154, https://doi.org/10.5194/nhess-2023-154, 2023
Revised manuscript accepted for NHESS
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Changes in sea-levels alone do not determine the evolution of coastal hazards. Coastal hazard changes should be assessed using additional factors describing geomorphological configurations, meteocean events types (storms, cyclones, long swells and tsunamis) and the marine environment (e. g., coral reef state and sea ice extent). The assessment completed here, at regional scale including the coasts of mainland and overseas France, highlights significant differences in hazard changes.
Zhang Haixia, Cheng Meng, and Fang Weihua
Nat. Hazards Earth Syst. Sci., 23, 2697–2717, https://doi.org/10.5194/nhess-23-2697-2023, https://doi.org/10.5194/nhess-23-2697-2023, 2023
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Simultaneous storm surge and waves can cause great damage due to cascading effects. Quantitative joint probability analysis is critical to determine their optimal protection design values. The joint probability of the surge and wave for the eastern coasts of Leizhou Peninsula and Hainan are estimated with a Gumbel copula based on 62 years of numerically simulated data, and the optimal design values under various joint return periods are derived using the non-linear programming method.
Clare Lewis, Tim Smyth, David Williams, Jess Neumann, and Hannah Cloke
Nat. Hazards Earth Syst. Sci., 23, 2531–2546, https://doi.org/10.5194/nhess-23-2531-2023, https://doi.org/10.5194/nhess-23-2531-2023, 2023
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Meteotsunami are globally occurring water waves initiated by atmospheric disturbances. Previous research has suggested that in the UK, meteotsunami are a rare phenomenon and tend to occur in the summer months. This article presents a revised and updated catalogue of 98 meteotsunami that occurred between 1750 and 2022. Results also demonstrate a larger percentage of winter events and a geographical pattern highlighting the
hotspotregions that experience these events.
Melissa Wood, Ivan D. Haigh, Quan Quan Le, Hung Nghia Nguyen, Hoang Ba Tran, Stephen E. Darby, Robert Marsh, Nikolaos Skliris, Joël J.-M. Hirschi, Robert J. Nicholls, and Nadia Bloemendaal
Nat. Hazards Earth Syst. Sci., 23, 2475–2504, https://doi.org/10.5194/nhess-23-2475-2023, https://doi.org/10.5194/nhess-23-2475-2023, 2023
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We used a novel database of simulated tropical cyclone tracks to explore whether typhoon-induced storm surges present a future flood risk to low-lying coastal communities around the South China Sea. We found that future climate change is likely to change tropical cyclone behaviour to an extent that this increases the severity and frequency of storm surges to Vietnam, southern China, and Thailand. Consequently, coastal flood defences need to be reviewed for resilience against this future hazard.
Sang-Guk Yum, Moon-Soo Song, and Manik Das Adhikari
Nat. Hazards Earth Syst. Sci., 23, 2449–2474, https://doi.org/10.5194/nhess-23-2449-2023, https://doi.org/10.5194/nhess-23-2449-2023, 2023
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This study performed analysis on typhoon-induced coastal morphodynamics for the Mokpo coast. Wetland vegetation was severely impacted by Typhoon Soulik, with 87.35 % of shoreline transects experiencing seaward migration. This result highlights the fact that sediment resuspension controls the land alteration process over the typhoon period. The land accretion process dominated during the pre- to post-typhoon periods.
Olle Räty, Marko Laine, Ulpu Leijala, Jani Särkkä, and Milla M. Johansson
Nat. Hazards Earth Syst. Sci., 23, 2403–2418, https://doi.org/10.5194/nhess-23-2403-2023, https://doi.org/10.5194/nhess-23-2403-2023, 2023
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We studied annual maximum sea levels in the Finnish coastal region. Our aim was to better quantify the uncertainty in them compared to previous studies. Using four statistical models, we found out that hierarchical models, which shared information on sea-level extremes across Finnish tide gauges, had lower uncertainty in their results in comparison with tide-gauge-specific fits. These models also suggested that the shape of the distribution for extreme sea levels is similar on the Finnish coast.
Jani Särkkä, Jani Räihä, Mika Rantanen, and Matti Kämäräinen
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-102, https://doi.org/10.5194/nhess-2023-102, 2023
Revised manuscript accepted for NHESS
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We study the relationship between tracks of low-pressure systems and related sea level extremes. We perform the studies by introducing a method to simulate sea levels using synthetic low-pressure systems. We test the method using sites located along the Baltic Sea coast. We find high extremes, where the sea level extreme reach up to 3.5 meters. In addition that, we add the maximal value of the mean level of the Baltic Sea (1 m) leading to sea level of 4.5 meters.
Alexey Androsov, Sven Harig, Natalia Zamora, Kim Knauer, and Natalja Rakowsky
EGUsphere, https://doi.org/10.5194/egusphere-2023-1365, https://doi.org/10.5194/egusphere-2023-1365, 2023
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Two numerical codes are used in a comparative analysis of the calculation of the tsunami wave due to an earthquake along the Peruvian coast. The comparison primarily evaluates the flow velocity fields in flooded areas. The relative importance of the various parts of the equations is determined, focusing on the nonlinear terms. The influence of the nonlinearity on the degree and volume of flooding, flow velocity and small-scale fluctuations is determined.
Christian Ferrarin, Florian Pantillon, Silvio Davolio, Marco Bajo, Mario Marcello Miglietta, Elenio Avolio, Diego S. Carrió, Ioannis Pytharoulis, Claudio Sanchez, Platon Patlakas, Juan Jesús González-Alemán, and Emmanouil Flaounas
Nat. Hazards Earth Syst. Sci., 23, 2273–2287, https://doi.org/10.5194/nhess-23-2273-2023, https://doi.org/10.5194/nhess-23-2273-2023, 2023
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The combined use of meteorological and ocean models enabled the analysis of extreme sea conditions driven by Medicane Ianos, which hit the western coast of Greece on 18 September 2020, flooding and damaging the coast. The large spread associated with the ensemble highlighted the high model uncertainty in simulating such an extreme weather event. The different simulations have been used for outlining hazard scenarios that represent a fundamental component of the coastal risk assessment.
Charline Dalinghaus, Giovanni Coco, and Pablo Higuera
Nat. Hazards Earth Syst. Sci., 23, 2157–2169, https://doi.org/10.5194/nhess-23-2157-2023, https://doi.org/10.5194/nhess-23-2157-2023, 2023
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Wave setup is a critical component of coastal flooding. Consequently, understanding and being able to predict wave setup is vital to protect coastal resources and the population living near the shore. Here, we applied machine learning to improve the accuracy of present predictors of wave setup. The results show that the new predictors outperform existing formulas demonstrating the capability of machine learning models to provide a physically sound description of wave setup.
Ina Teutsch, Markus Brühl, Ralf Weisse, and Sander Wahls
Nat. Hazards Earth Syst. Sci., 23, 2053–2073, https://doi.org/10.5194/nhess-23-2053-2023, https://doi.org/10.5194/nhess-23-2053-2023, 2023
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Rogue waves exceed twice the significant wave height. They occur more often than expected in the shallow waters off Norderney. When applying a nonlinear Fourier transform for the Korteweg–de Vries equation to wave data from Norderney, we found differences in the soliton spectra of time series with and without rogue waves. A strongly outstanding soliton in the spectrum indicated an enhanced probability for rogue waves. We could attribute spectral solitons to the measured rogue waves.
Philipp Heinrich, Stefan Hagemann, Ralf Weisse, Corinna Schrum, Ute Daewel, and Lidia Gaslikova
Nat. Hazards Earth Syst. Sci., 23, 1967–1985, https://doi.org/10.5194/nhess-23-1967-2023, https://doi.org/10.5194/nhess-23-1967-2023, 2023
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High seawater levels co-occurring with high river discharges have the potential to cause destructive flooding. For the past decades, the number of such compound events was larger than expected by pure chance for most of the west-facing coasts in Europe. Additionally rivers with smaller catchments showed higher numbers. In most cases, such events were associated with a large-scale weather pattern characterized by westerly winds and strong rainfall.
Alexander Böhme, Birgit Gerkensmeier, Benedikt Bratz, Clemens Krautwald, Olaf Müller, Nils Goseberg, and Gabriele Gönnert
Nat. Hazards Earth Syst. Sci., 23, 1947–1966, https://doi.org/10.5194/nhess-23-1947-2023, https://doi.org/10.5194/nhess-23-1947-2023, 2023
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External surges in the North Sea are caused by low-pressure cells travelling over the northeast Atlantic. They influence extreme water levels on the German coast and have to be considered in the design process of coastal defence structures. This study collects data about external surges from 1995–2020 and analyses their causes, behaviours and potential trends. External surges often occur less than 72 h apart, enabling a single storm surge to be influenced by more than one external surge.
Kenta Tozato, Shuji Moriguchi, Shinsuke Takase, Yu Otake, Michael R. Motley, Anawat Suppasri, and Kenjiro Terada
Nat. Hazards Earth Syst. Sci., 23, 1891–1909, https://doi.org/10.5194/nhess-23-1891-2023, https://doi.org/10.5194/nhess-23-1891-2023, 2023
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This study presents a framework that efficiently investigates the optimal placement of facilities probabilistically based on advanced numerical simulation. Surrogate models for the numerical simulation are constructed using a mode decomposition technique. Monte Carlo simulations using the surrogate models are performed to evaluate failure probabilities. Using the results of the Monte Carlo simulations and the genetic algorithm, optimal placements can be investigated probabilistically.
Job C. M. Dullaart, Sanne Muis, Hans de Moel, Philip J. Ward, Dirk Eilander, and Jeroen C. J. H. Aerts
Nat. Hazards Earth Syst. Sci., 23, 1847–1862, https://doi.org/10.5194/nhess-23-1847-2023, https://doi.org/10.5194/nhess-23-1847-2023, 2023
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Coastal flooding is driven by storm surges and high tides and can be devastating. To gain an understanding of the threat posed by coastal flooding and to identify areas that are especially at risk, now and in the future, it is crucial to accurately model coastal inundation and assess the coastal flood hazard. Here, we present a global dataset with hydrographs that represent the typical evolution of an extreme sea level. These can be used to model coastal inundation more accurately.
Elin Andrée, Jian Su, Morten Andreas Dahl Larsen, Martin Drews, Martin Stendel, and Kristine Skovgaard Madsen
Nat. Hazards Earth Syst. Sci., 23, 1817–1834, https://doi.org/10.5194/nhess-23-1817-2023, https://doi.org/10.5194/nhess-23-1817-2023, 2023
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When natural processes interact, they may compound each other. The combined effect can amplify extreme sea levels, such as when a storm occurs at a time when the water level is already higher than usual. We used numerical modelling of a record-breaking storm surge in 1872 to show that other prior sea-level conditions could have further worsened the outcome. Our research highlights the need to consider the physical context of extreme sea levels in measures to reduce coastal flood risk.
Ekaterina Didenkulova, Ira Didenkulova, and Igor Medvedev
Nat. Hazards Earth Syst. Sci., 23, 1653–1663, https://doi.org/10.5194/nhess-23-1653-2023, https://doi.org/10.5194/nhess-23-1653-2023, 2023
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The paper is dedicated to freak wave accidents which happened in the world ocean in 2005–2021 and that were described in mass media sources. The database accounts for 429 events, all of which resulted in ship or coastal and offshore structure damage and/or human losses. In agreement with each freak wave event, we put background wave and wind conditions extracted from the climate reanalysis ERA5. We analyse their statistics and discuss the favourable conditions for freak wave occurrence.
Havu Pellikka, Milla M. Johansson, Maaria Nordman, and Kimmo Ruosteenoja
Nat. Hazards Earth Syst. Sci., 23, 1613–1630, https://doi.org/10.5194/nhess-23-1613-2023, https://doi.org/10.5194/nhess-23-1613-2023, 2023
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We explore the rate of past and future sea level rise at the Finnish coast, northeastern Baltic Sea, in 1901–2100. For this analysis, we use tide gauge observations, modelling results, and a probabilistic method to combine information from several sea level rise projections. We provide projections of local mean sea level by 2100 as probability distributions. The results can be used in adaptation planning in various sectors with different risk tolerance, e.g. land use planning or nuclear safety.
Carlos Corela, Afonso Loureiro, José Luis Duarte, Luis Matias, Tiago Rebelo, and Tiago Bartolomeu
Nat. Hazards Earth Syst. Sci., 23, 1433–1451, https://doi.org/10.5194/nhess-23-1433-2023, https://doi.org/10.5194/nhess-23-1433-2023, 2023
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We show that ocean-bottom seismometers are controlled by bottom currents, but these are not always a function of the tidal forcing. Instead we suggest that the ocean bottom has a flow regime resulting from two possible contributions: the permanent low-frequency bottom current and the tidal current along the full tidal cycle, between neap and spring tides. In the short-period noise band the ocean current generates harmonic tremors that corrupt the dataset records.
Chen Chen, Charles Koll, Haizhong Wang, and Michael K. Lindell
Nat. Hazards Earth Syst. Sci., 23, 733–749, https://doi.org/10.5194/nhess-23-733-2023, https://doi.org/10.5194/nhess-23-733-2023, 2023
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This paper uses empirical-data-based simulation to analyze how to evacuate efficiently from disasters. We find that departure delay time and evacuation decision have significant impacts on evacuation results. Evacuation results are more sensitive to walking speed, departure delay time, evacuation participation, and destinations than to other variables. This model can help authorities to prioritize resources for hazard education, community disaster preparedness, and resilience plans.
Ariadna Martín, Angel Amores, Alejandro Orfila, Tim Toomey, and Marta Marcos
Nat. Hazards Earth Syst. Sci., 23, 587–600, https://doi.org/10.5194/nhess-23-587-2023, https://doi.org/10.5194/nhess-23-587-2023, 2023
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Tropical cyclones (TCs) are among the potentially most hazardous phenomena affecting the coasts of the Caribbean Sea. This work simulates the coastal hazards in terms of sea surface elevation and waves that originate through the passage of these events. A set of 1000 TCs have been simulated, obtained from a set of synthetic cyclones that are consistent with present-day climate. Given the large number of hurricanes used, robust values of extreme sea levels and waves are computed along the coasts.
An-Chi Cheng, Anawat Suppasri, Kwanchai Pakoksung, and Fumihiko Imamura
Nat. Hazards Earth Syst. Sci., 23, 447–479, https://doi.org/10.5194/nhess-23-447-2023, https://doi.org/10.5194/nhess-23-447-2023, 2023
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Consecutive earthquakes occurred offshore of southern Taiwan on 26 December 2006. This event revealed unusual tsunami generation and propagation, as well as unexpected consequences for the southern Taiwanese coast (i.e., amplified waves and prolonged durations). This study aims to elucidate the source characteristics of the 2006 tsunami and the important behaviors responsible for tsunami hazards in Taiwan such as wave trapping and shelf resonance.
Jean Roger, Bernard Pelletier, Aditya Gusman, William Power, Xiaoming Wang, David Burbidge, and Maxime Duphil
Nat. Hazards Earth Syst. Sci., 23, 393–414, https://doi.org/10.5194/nhess-23-393-2023, https://doi.org/10.5194/nhess-23-393-2023, 2023
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On 10 February 2021 a magnitude 7.7 earthquake occurring at the southernmost part of the Vanuatu subduction zone triggered a regional tsunami that was recorded on many coastal gauges and DART stations of the south-west Pacific region. Beginning with a review of the tectonic setup and its implication in terms of tsunami generation in the region, this study aims to show our ability to reproduce a small tsunami with different types of rupture models and to discuss a larger magnitude 8.2 scenario.
Kathrin Wahle, Emil V. Stanev, and Joanna Staneva
Nat. Hazards Earth Syst. Sci., 23, 415–428, https://doi.org/10.5194/nhess-23-415-2023, https://doi.org/10.5194/nhess-23-415-2023, 2023
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Knowledge of what causes maximum water levels is often key in coastal management. Processes, such as storm surge and atmospheric forcing, alter the predicted tide. Whilst most of these processes are modeled in present-day ocean forecasting, there is still a need for a better understanding of situations where modeled and observed water levels deviate from each other. Here, we will use machine learning to detect such anomalies within a network of sea-level observations in the North Sea.
Chuan Li, H. Tuba Özkan-Haller, Gabriel García Medina, Robert A. Holman, Peter Ruggiero, Treena M. Jensen, David B. Elson, and William R. Schneider
Nat. Hazards Earth Syst. Sci., 23, 107–126, https://doi.org/10.5194/nhess-23-107-2023, https://doi.org/10.5194/nhess-23-107-2023, 2023
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In this work, we examine a set of observed extreme, non-earthquake-related and non-landslide-related wave runup events. Runup events with similar characteristics have previously been attributed to trapped waves, atmospheric disturbances, and abrupt breaking of long waves. However, we find that none of these mechanisms were likely at work in the observations we examined. We show that instead, these runup events were more likely due to energetic growth of bound infragravity waves.
Shan Liu, Xianwu Shi, Qiang Liu, Jun Tan, Yuxi Sun, Qingrong Liu, and Haoshuang Guo
Nat. Hazards Earth Syst. Sci., 23, 127–138, https://doi.org/10.5194/nhess-23-127-2023, https://doi.org/10.5194/nhess-23-127-2023, 2023
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This study proposes a quantitative method for the determination of warning water levels. The proposed method is a multidimensional scale, centered on the consideration of various factors that characterize various coastlines. The implications of our study are not only scientific, as we provide a method for water level determination that is rooted in the scientific method (and reproducible across various contexts beyond China), but they are also deeply practical.
Jaap H. Nienhuis, Jana R. Cox, Joey O'Dell, Douglas A. Edmonds, and Paolo Scussolini
Nat. Hazards Earth Syst. Sci., 22, 4087–4101, https://doi.org/10.5194/nhess-22-4087-2022, https://doi.org/10.5194/nhess-22-4087-2022, 2022
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Humans build levees to protect themselves against floods. We need to know where they are to correctly predict flooding, for example from sea level rise. Here we have looked through documents to find levees, and checked that they exist using satellite imagery. We developed a global levee map, available at www.opendelve.eu, and we found that 24 % of people in deltas are protected by levees.
Alec Torres-Freyermuth, Gabriela Medellín, Jorge A. Kurczyn, Roger Pacheco-Castro, Jaime Arriaga, Christian M. Appendini, María Eugenia Allende-Arandía, Juan A. Gómez, Gemma L. Franklin, and Jorge Zavala-Hidalgo
Nat. Hazards Earth Syst. Sci., 22, 4063–4085, https://doi.org/10.5194/nhess-22-4063-2022, https://doi.org/10.5194/nhess-22-4063-2022, 2022
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Barrier islands in tropical regions are prone to coastal flooding and erosion during hurricane events. The Yucatán coast was impacted by hurricanes Gamma and Delta. Inner shelf, coastal, and inland observations were acquired. Beach morphology changes show alongshore gradients. Flooding occurred on the back barrier due to heavy inland rain and the coastal aquifer's confinement. Modeling systems failed to reproduce the coastal hydrodynamic response due to uncertainties in the boundary conditions.
Panagiotis Athanasiou, Ap van Dongeren, Alessio Giardino, Michalis Vousdoukas, Jose A. A. Antolinez, and Roshanka Ranasinghe
Nat. Hazards Earth Syst. Sci., 22, 3897–3915, https://doi.org/10.5194/nhess-22-3897-2022, https://doi.org/10.5194/nhess-22-3897-2022, 2022
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Sandy dunes protect the hinterland from coastal flooding during storms. Thus, models that can efficiently predict dune erosion are critical for coastal zone management and early warning systems. Here we develop such a model for the Dutch coast based on machine learning techniques, allowing for dune erosion estimations in a matter of seconds relative to available computationally expensive models. Validation of the model against benchmark data and observations shows good agreement.
Cuneyt Yavuz, Kutay Yilmaz, and Gorkem Onder
Nat. Hazards Earth Syst. Sci., 22, 3725–3736, https://doi.org/10.5194/nhess-22-3725-2022, https://doi.org/10.5194/nhess-22-3725-2022, 2022
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Even if the coincidence of flood and tsunami hazards may be experienced once in a blue moon, it should also be investigated due to the uncertainty of the time of occurrence of these natural hazards. The objective of this study is to reveal a statistical methodology to evaluate the aggregate potential hazard levels due to flood hazards with the presence of earthquake-triggered tsunamis. The proposed methodology is applied to Fethiye city, located on the Western Mediterranean coast of Turkey.
Damiano Baldan, Elisa Coraci, Franco Crosato, Maurizio Ferla, Andrea Bonometto, and Sara Morucci
Nat. Hazards Earth Syst. Sci., 22, 3663–3677, https://doi.org/10.5194/nhess-22-3663-2022, https://doi.org/10.5194/nhess-22-3663-2022, 2022
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Extreme-event analysis is widely used to provide information for the design of coastal protection structures. Non-stationarity due to sea level rise can affect such estimates. Using different methods on a long time series of sea level data, we show that estimates of the magnitude of extreme events in the future can be inexact due to relative sea level rise. Thus, considering non-stationarity is important when analyzing extreme-sea-level events.
Umesh Pranavam Ayyappan Pillai, Nadia Pinardi, Ivan Federico, Salvatore Causio, Francesco Trotta, Silvia Unguendoli, and Andrea Valentini
Nat. Hazards Earth Syst. Sci., 22, 3413–3433, https://doi.org/10.5194/nhess-22-3413-2022, https://doi.org/10.5194/nhess-22-3413-2022, 2022
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The study presents the application of high-resolution coastal modelling for wave hindcasting on the Emilia-Romagna coastal belt. The generated coastal databases which provide an understanding of the prevailing wind-wave characteristics can aid in predicting coastal impacts.
Cited articles
Auriac, A., Whitehouse, P. L., Bentley, M. J., Patton, H., Lloyd, J. M., and
Hubbard, A.: Glacial isostatic adjustment associated with the Barents Sea
ice sheet: a modelling inter-comparison, Quaterny Sci. Rev., 147, 122–135,
https://doi.org/10.1016/j.quascirev.2016.02.011, 2016.
Bécel, A., Shillington, D. J., Delescluse, M., Nedimović, M. R.,
Abers, G. A., Saffer, D. M., and Kuehn, H.: Tsunamigenic structures in a
creeping section of the Alaska subduction zone, Nat. Geosci., 10,
609–613, https://doi.org/10.1038/ngeo2990, 2017.
Bellwald, B., Hjelstuen, B. O., Sejrup, H. P., and Haflidason, H.:
Postglacial mass movements and depositional environments in a high-latitude
fjord system–Hardangerfjorden, Western Norway, Mar. Geol., 379, 157–175,
https://doi.org/10.1016/j.margeo.2016.06.002, 2016.
Berkhoff, J. C. W.: Computation of combined refraction – diffraction, Coastal Engineering Proceedings, 1, 471–490, https://doi.org/10.9753/icce.v13.23, 1972.
Berndt, C., Brune, S., Nisbet, E., Zschau, J., and Sobolev, S. V.: Tsunami
modelling of a submarine landslide in the Fram Strait, Geochem. Geophys., 10, Q04009, https://doi.org/10.1029/2008GC002292, 2009.
Blikra, L.H., Longva, O., Harbitz, C., and Løvholt, F.: Quantification of rock-avalanche and tsunami hazard in Storfjorden, western Norway, in: Landslides and Avalanches, ICFL Norway, edited by: Senneset, K., Flaate, K., and Larsen, J. O., Taylor and Francis, London, IK, 57–64, ISBN 0415386780, 2005.
Böhme, M., Oppikofer, T., Longva, O., Jaboyedoff, M., Hermanns, R. L.,
and Derron, M. H: Analyses of past and present rock slope instabilities in a
fjord valley: Implications for hazard estimations, Geomorphology, 248,
464–474, https://doi.org/10.1016/j.geomorph.2015.06.045, 2015.
Bondevik, S., Mangerud, J., Dawson, S., Dawson, and A., and Lohne, Ø.:
Record-breaking height for 8000-year-old tsunami in the North Atlantic, EOS,
84, 289–297, https://doi.org/10.1029/2003EO310001, 2003.
Bondevik, S., Stormo, S. K., and Skjerdal, G.: Green mosses date the
Storegga tsunami to the chilliest decades of the 8.2 ka cold event, Quaterny Sci. Rev., 45, 1–6, https://doi.org/10.1016/j.quascirev.2012.04.020, 2012.
Brunet, M., Moretti, L., Le Friant, A., Mangeney, A., Fernández Nieto, E. D., and Bouchut, F.: Numerical simulation of the 30–45 ka
debris avalanche flow of Montagne Pelée volcano, Martinique: from
volcano flank collapse to submarine emplacement, Nat. Hazards, 87,
1189–1222, https://doi.org/10.1007/s11069-017-2815-5, 2017.
Bugge, T., Befring, S., Belderson, R. H., Eidvin, T., Jansen, E., Kenyon, N.,
Holtedahl, H., and Sejrup, H. P.: A giant three-stage submarine slide off
Norway, Geo-Mar. Lett., 7, 191–198, 1987.
Butt, F. A., Elverhøi, A., Solheim, A., and Forsberg, C. F.: Deciphering
late Cenozoic development of the western Svalbard Margin from ODP Site 986
results, Mar. Geol., 169, 373–390, https://doi.org/10.1016/S0025-3227(00)00088-8,
2000.
Canals, M., Lastras, G., Urgeles, R., Casamor, J. L., Mienert, J., Cattaneo,
A., De Batist, M., Haflidason, H., Imbo, Y., Laberg, J. S., Locat, J., Long,
D., Longva, O., Masson, D. G., Sultan, N., Trincardi, F., and Bryn, P.:
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor
geophysical data: case studies from the COSTA project, Mar. Geol., 213,
9–72, https://doi.org/10.1016/j.margeo.2004.10.001, 2004.
Casas, D., Ercilla, G., García, M., Yenes, M., and Estrada, F.:
Post-rift sedimentary evolution of the Gebra Debris Valley. A submarine
slope failure system in the Central Bransfield Basin (Antarctica), Mar. Geol.,
340, 16–29, https://doi.org/10.1016/j.margeo.2013.04.011, 2013.
Casas, D., Chiocci, F., Casalbore, D., Ercilla, G., and De Urbina, J. O.:
Magnitude-frequency distribution of submarine landslides in the
Gioia Basin (southern Tyrrhenian Sea), Geo-Mar. Lett., 36, 405–414, 2016.
Castro, M. J., Ortega, S., De la Asuncion, M., Mantas, J. M., and Gallardo,
J. M.: GPU computing for shallow water flow simulation based on finite
volume schemes, C. R. Mec., 339, 165–184, https://doi.org/10.1016/j.crme.2010.12.004, 2011.
Castro Díaz, M. J., and Fernández-Nieto, E.: A class of computationally
fast first order finite volume solvers: PVM methods, SIAM, J. Sci. Comput.,
34, A2173–A2196, https://doi.org/10.1137/100795280, 2012.
Chiocci, F. L. and Casalbore, D.: Unexpected fast rate of
morphological evolution of geologically-active continental margins during
Quaternary: Examples from selected areas in the Italian seas, Mar.
Petrol. Geol., 82, 154–162, 2017.
Chiocci, F. L. and Ridente, D.: Regional-scale seafloor mapping and
geohazard assessment. The experience from the Italian project MaGIC (Marine
Geohazards along the Italian Coasts), Mar. Geophys. Res., 32, 13–23, https://doi.org/10.1007/s11001-011-9120-6, 2011.
Cofaigh, C. Ó., Taylor, J., Dowdeswell, J. A., and Pudsey, C. J.: Palaeo-ice streams, trough mouth fans and high‐latitude continental slope sedimentation, Boreas, 32, 37–55, https://doi.org/10.1080/03009480310001858, 2003.
CSIC: Oceanography Cruise and Data Catalogue of CSIC-UTM/Marine Technology Unit, CSIC [data set], https://doi.org/10.20351/29HE20070802, 2018.
Dietrich, A. and Krautblatter, M.: Deciphering controls for debris-flow
erosion derived from a LiDAR-recorded extreme event and a calibrated
numerical model, Earth Surf. Proc. Land., 44, 1346–1361, https://doi.org/10.1002/esp.4578, 2019.
Dowdeswell, J. A., Ottesen, D., Evans, J., Cofaigh, C. Ó., and Anderson, J. B.: Submarine glacial landforms and rates of ice-stream collapse, Geology, 36, 819–822, https://doi.org/10.1130/G24808A.1, 2008.
Eck, M. and Hoppe, H.: Automatic reconstruction of B-spline surfaces of
arbitrary topological type, in: Proceedings of the 23rd annual conference on
Computer Graphics and Interactive Techniques, 325–334, https://doi.org/10.1145/237170.237271, 1996.
EDANYA Research Group:
Video 1 – Storfjorden landslide tsunami, TIB AV-Portal [video], https://doi.org/10.5446/56981, 2022a.
EDANYA Research Group:
Video 2 – Storfjorden landslide tsunami propagation, TIB AV-Portal [video],
https://doi.org/10.5446/56982, 2022b.
Eiken, O.: Seismic Atlas of Western Svalbard, Norsk Polarinstitutts
Meddelelser, 130, 73, ISBN 82-7666-067-3, 1994.
Elverhøi, A., De Blasio, F. V., Butt, F. A., Issler, D., Harbitz, C., Engvik, L., and Marr, J.: Submarine mass-wasting on glacially-influenced continental slopes: processes and dynamics. Geological Society, London, Special Publications, 203, 73–87, 2002.
Engen, Ø., Faleide, J. I., and Dyreng, T. K.: Opening of the Fram Strait
gateway: A review of plate tectonic constraints, Tectonophysics, 450,
51–69, https://doi.org/10.1016/j.tecto.2008.01.002, 2008.
Ercilla, G., Casas, D., Alonso, B., Casalbore, D., Galindo-Zaldívar, J., García-Gil, S., Martorelli, E., Vázquez, J. T., Azpiroz-Zabala, M., DoCouto, D., Estrada, F., Fernández-Puga, M. C., González-Castillo, L., González-Vida, J.M., Idárraga-García, J., Juan, C., Macías, J., Madarieta-Txurruka, A., Nespereira, J., Palomino, D., Sánchez-Guillamón, O., Tendero-Salmerón, V., Teixeira, M., Valencia, J., and Yenes, M.: Offshore Geological Hazards:
Charting the Course of Progress and
Future Directions, Oceans, 2,
393–429, https://doi.org/10.3390/oceans2020023, 2021.
Ercilla, G., Casas, D., Alonso, B., Casalbore, D., Estrada, F., Idárraga-García, J., López-González, N., Pedrosa, M., Teixeira, M., Sánchez-Guillamón, O., Azpiroz-Zabala, M., Bárcenas, P., Chiocci, F. L., García, M., Galindo-Zaldívar, J., Geyer, A., Gómez-Ballesteros, M., Juan, C., Martorelli, E., and Yenes,
M.: Deep Sea Sedimentation, edited by: Jack, J. and Shroder, F., in: Treatise on Geomorphology (Second Edition), Academic Press, 960–988, https://doi.org/10.1016/B978-0-12-818234-5.00129-2,
ISBN 9780128182352, 2022.
Escalante, C., Morales de Luna, T., and Castro, M. J.: Non-hydrostatic
pressure shallow flows: GPU implementation using finite volume and finite
difference scheme, Appl. Math. Comput., 338, 631–659, https://doi.org/10.1016/j.amc.2018.06.035, 2018.
Escalante, C., Dumbser, M., and Castro, M. J.: An efficient hyperbolic
relaxation system for dispersive non-hydrostatic water waves and its
solution with high order discontinuous Galerkin schemes, J.
Comput. Phys., 394, 385–416, https://doi.org/10.1016/j.jcp.2019.05.035, 2019.
Estrada, F., González-Vida, J. M., Peláez, J. A.,
Galindo-Zaldívar, J., Ortega, S., Macías, J., and Ercilla, G.:
Tsunami generation potential of a strike-slip fault tip in the westernmost
Mediterranean, Sci. Rep.-UK, 11, 1–9, https://doi.org/10.1038/s41598-021-95729-6, 2021.
Evans, S. G., Bishop, N. F., Smoll, L. F., Murillo, P. V., Delaney, K. B., and Oliver-Smith, A.: A re-examination of the mechanism and human impact of catastrophic mass flows originating on Nevado Huascarán, Cordillera Blanca, Peru in 1962 and 1970, Eng. Geol., 108, 96–118, https://doi.org/10.1016/j.enggeo.2009.06.020, 2009.
Faleide, J. I., Solheim, A., Fiedler, A., Hjelstuen, B. O., Andersen, E. S., and Vaneste, K.: Late Cenozoic evolution of the western Barents Sea-Svaldbard continental margin, Global Planet. Change, 12, 53–74, https://doi.org/10.1016/0921-8181(95)00012-7, 1996.
Faleide, J. I., Vågnes, E., and Gudlaugsson, S. T.: Late
Mesozoic–Cenozoic evolution of the southwestern Barents Sea in a regional
rift-shear tectonic setting, Mat. Pet. Geol., 10, 186–214, https://doi.org/10.1016/0264-8172(93)90104-Z, 1993.
Faleide, J. I., Tsikalas, F., Breivik, A. J., Mjelde, R., Ritzmann, O.,
Wilson, J., and Eldholm, O.: Structure and evolution of the continental
margin off Norway and the Barents Sea, J. Int. Geosci., 31, 82–91, https://doi.org/10.18814/epiiugs/2008/v31i1/012, 2008.
Fernández-Nieto, E. D., Bouchut, F., Bresch, D. Castro., and M. J.,
Mangeney, A.: A new Savage–Hutter type model for submarine avalanches and
generated tsunami, J. Comput. Phys, 227, 7720–775, https://doi.org/10.1016/j.jcp.2008.04.039, 2008.
Fernandez-Nieto, E., Parisot, M., Penel, Y., and Sainte-Marie, J.: A
hierarchy of dispersive layer-averaged approximations of Euler equations for
free surface flows, Commun. Math. Sci., 16, 1169–1202,
2018.
Fiedler, A. and Faleide, J. I.: Cenozoic sedimentation along the southwestern
Barents Sea margin in relation to uplift and erosion of the shelf, Global
Planet. Change, 12, 75–93, https://doi.org/10.1016/0921-8181(95)00013-5, 1996.
Fine, I. V., Rabinovich, A. B., Bornhold, B. D., Thomson, R. E., and
Kulikov, E. A.: The Grand Banks landslide-generated tsunami of November 18,
1929: preliminary analysis and numerical modelling, Mar. Geol., 215,
45–57, https://doi.org/10.1016/j.margeo.2004.11.007, 2005.
Førland, E. J., Jacobsen, J. K. S., Denstadli, J. M., Lohmann, M.,
Hanssen-Bauer, I., Hygen, H. O., and Tømmervik, H.: Cool weather tourism
under global warming: Comparing Arctic summer tourists' weather preferences
with regional climate statistics and projections, Tourism Manage., 36,
567–579, https://doi.org/10.1016/j.tourman.2012.09.002, 2013.
Fryer, G. J., Watts, P., and Pratson, L. F.: Source of the great tsunami of
1 April 1946: a landslide in the upper Aleutian forearc, Mar. Geol.,
203, 201–218, https://doi.org/10.1016/S0025-3227(03)00305-0, 2004.
García, M., Ercilla, G., and Alonso, B.: Morphology and sedimentary
systems in the Central Bransfield Basin, Antarctic Peninsula: sedimentary
dynamics from shelf to basin, Basin Res., 21, 295–314, https://doi.org/10.1111/j.1365-2117.2008.00386.x, 2009.
García, M., Ercilla, G., Alonso, B., Casas, D., and Dowdeswell, J. A.:
Sediment lithofacies, processes and sedimentary models in the Central
Bransfield Basin, Antarctic Peninsula, since the Last Glacial Maximum, Mar.
Geol., 290, 1–16, https://doi.org/10.1016/j.margeo.2011.10.006, 2011.
González-Vida, J. M., Macías, J., Castro, M. J., Sánchez-Linares, C., de la Asunción, M., Ortega-Acosta, S., and Arcas, D.: The Lituya Bay landslide-generated mega-tsunami – numerical simulation and sensitivity analysis, Nat. Hazards Earth Syst. Sci., 19, 369–388, https://doi.org/10.5194/nhess-19-369-2019, 2019.
Haflidason, H., Sejrup, H. P., Nygård, A., Mienert, J., Bryn, P., Lien,
R., and Masson, D.: The Storegga Slide: architecture, geometry and slide
development, Mar. Geol., 213, 201–234, https://doi.org/10.1016/j.margeo.2004.10.007, 2004.
Haflidason, H., Lien, R., Sejrup, H. P., Forsberg, C. F., and Bryn, P.: The
dating and morphometry of the Storegga Slide, Mar. Petrol. Geol., 22, 123–136, https://doi.org/10.1016/j.marpetgeo.2004.10.008, 2005.
Hampel, A., Hetzel, R., Maniatis, G., and Karow, T.: Three-dimensional
numerical modelling of slip rate variations on normal and thrust fault
arrays during ice cap growth and melting, J. Geophys. Res., 114, 406,
https://doi.org/10.1029/2008JB006113, 2009.
Harbitz, C. B., Løvholt, F., Pedersen, G., and Masson, D. G.: Mechanisms
of tsunami generation by submarine landslides: a short review, N. J. Geol.,
86, 255–264, 2006.
Huggel, C., Zgraggen-Oswald, S., Haeberli, W., Kääb, A., Polkvoj, A., Galushkin, I., and Evans, S. G.: The 2002 rock/ice avalanche at Kolka/Karmadon, Russian Caucasus: assessment of extraordinary avalanche formation and mobility, and application of QuickBird satellite imagery, Nat. Hazards Earth Syst. Sci., 5, 173–187, https://doi.org/10.5194/nhess-5-173-2005, 2005.
Iglesias, O., Lastras, G., Canals, M., Olabarrieta, M., Gonzalez, M.,
Aniel-Quiroga, Í., and De Mol, B.: The BIG'95 submarine
landslide–generated tsunami: a numerical simulation, J.
Geol., 120, 31–48, https://doi.org/10.1086/662718, 2012.
Imamura, F., Boret, S. P., Suppasri, A., and Muhari, A.: Recent occurrences
of serious tsunami damage and the future challenges of tsunami disaster risk
reduction, Progress in Disaster Science, 1, 100009, https://doi.org/10.1016/j.pdisas.2019.100009, 2019.
Jakobsson, M., Mayer, L., Coakley, B., Dowdeswell, J. A., Forbes, S., Fridman, B., Weatherall, P., Hodnesdal, H., Noormets, R., Pedersen, R., Rebesco, M., Scheke, H. W., Zarayskaya, Y., Accettella, D., Armstrong, Anderson, R. M., Bienhoff, P., Camerlenghi, A., Church, I., Edwards, M., Gardner, J. V., Hall, J. K., Hell, B., Hestvik, O., Krstoffersen, Y., Marcussen, C., Mohammad, R., Mosher, D., Nghiem, S. V., Pedrosa, M. T., Trabaglini, P. G., and Weatherall, P.: The International Bathymetric Chart of the Arctic Ocean (IBCAO) version 3.0, Geophys. Res. Lett., 39, L12609, https://doi.org/10.1029/2012GL052219, 2012.
Knies, J., Matthiessen, J., Vogt, C., Laberg, J. S., Hjelstuen, B. O.,
Smelror, M., Larsen, E., Andreassen, K., Eidvin, T., Vorren, T. O.: The
Plio-Pleistocene glaciation of the Barents Sea–Svalbard region: a new model
based on revised chronostratigraphy, Quaterny Sci. Rev., 28, 812–829,
https://doi.org/10.1016/j.quascirev.2008.12.002, 2009.
Kvalstad, T. J., Andresen, L., Forsberg, C. F., Berg, K., Bryn, P., and Wangen, M.: The Storegga slide: evaluation of triggering sources and slide mechanics, Marine and Petroleum Geology, Elsevier, 22, 245–256, https://doi.org/10.1016/j.marpetgeo.2004.10.019, 2005.
Laberg, J. S. and Vorren, T. O.: A Late Pleistocene submarine slide on the
Bear Island Trough Mouth Fan, Geo-Mar. Lett., 13, 227–234,
https://doi.org/10.1007/BF01207752, 1993.
Laberg, J. S., Vorren, T. O., and Knutsen, S. M.: The Lofoten contourite drift off Norway, Mar. Geol., 159, 1–6, https://doi.org/10.1016/S0025-3227(98)00198-4, 1999.
Laberg, J. S., Vorren, T.O., Dowdeswell, J. A., Kenyon, N. H., and Taylor, J.:
The Andøya Slide and the Andøya Canyon, north-eastern
Norwegian–Greenland Sea, Mar. Geol., 162, 259–275, 2000.
Laberg, J. S., Vorren, T. O., Mienert, J., Evans, D., Lindberg, B., Ottesen, D., and Henriksen, S.: Late Quaternary palaeoenvironment and chronology in the Trænadjupet Slide area offshore Norway, Mar. Geol., 188, 35–60, https://doi.org/10.1016/S0025-3227(02)00274-8, 2002.
Lee, H. J.: Timing of occurrence of large submarine landslides on the
Atlantic Ocean margin, Mar. Geol., 264, 53–64, https://doi.org/10.1016/j.margeo.2008.09.009, 2009.
Lee, S., Wolberg, G., and Shin, S. Y.: Scattered data interpolation with
multilevel B-splines, IEEE T. Vis. Comput.
Gr., 3, 228–244, https://doi.org/10.1109/2945.620490, 1997.
L'Heureux, J. S., Vanneste, M., Rise, L., Brendryen, J., Forsberg, C. F.,
Nadim, F., Longva, O., Chand, S., Kvalstad, T. J., and Haflidason, H.:
Stability, mobility and failure mechanism for landslides at the upper
continental slope off Vesterålen, Norway, Mar. Geol., 346, 192–207,
https://doi.org/10.1016/j.margeo.2013.09.009, 2013.
León, R., Llorente, M., and Giménez-Moreno, C. J.: Marine Gas
Hydrate Geohazard Assessment on the European Continental Margins. The Impact
of Critical Knowledge Gaps, Appl. Sci., 11, 2865, https://doi.org/10.3390/app11062865, 2021.
Lindberg, B., Laberg, J. S., and Vorren, T. O.: The Nyk Slide–morphology,
progression, and age of a partly buried submarine slide offshore northern
Norway, Mar. Geol., 213, 277–289, https://doi.org/10.1016/j.margeo.2004.10.010,
2004.
Llopart, J.: Storfjorden Trough Mouth Fan (Western Barents Sea): Slope
Failures in Polar Continental Margins; Significance of Stress Changes and
Fluid Migration Induced by Glacial Cycles, PhD thesis, Universitat de
Barcelona, 231 pp., http://hdl.handle.net/2445/108581 (last access: 20 September 2022), 2016.
Llopart, J., Urgeles, R., Camerlenghi, A., Lucchi, R. G., Rebesco, M., and De
Mol, B.: Late Quaternary development of the Storfjorden and Kveithola Trough
Mouth Fans, northwestern Barents Sea, Quaterny Sci. Rev. 129, 68–84,
https://doi.org/10.1016/j.quascirev.2015.10.002, 2015.
Llopart, J., Urgeles, R., Forsberg, C. F., Camerlenghi, A., Vanneste, M.,
Rebesco, M., and Lantzsch, H.: Fluid flow and pore pressure development
throughout the evolution of a trough mouth fan, western Barents Sea, Basin
Res., 31, 487–513, https://doi.org/10.1111/bre.12331, 2019.
Løvholt, F., Pedersen, G., Harbitz, C. B., Glimsdal, S., and Kim, J.: On
the characteristics of landslide tsunamis, Philos. T. R. Soc.
A, 373, 2053, https://doi.org/10.1098/rsta.2014.0376, 2015.
Løvholt, F., Glimsdal, S., and Harbitz, C. B.: On the landslide tsunami
uncertainty and hazard, Landslides, 17, 2301–2315, https://doi.org/10.1007/s10346-020-01429-z, 2020.
Lucchi, R. G., Pedrosa, M. T., Camerlenghi, A., Urgeles, R., De Mol, B., and
Rebesco, M.: Recent submarine landslides on the continental slope of
Storfjorden and Kveithola Trough-Mouth Fans (North West Barents Sea), in:
Submarine Mass Movement and Their
Consequences, Advances in Natural and Technological Hazards Research, edited by: Yamada, Y., Kawamura, K., Ikehara, K., Ogawa, Y., Urgeles, R., Mosher, D.,
Chaytor, J., and Strasser, M., 31,
Springer, Dordrecht, the Netherlands, 735–745, https://doi.org/10.1007/978-94-007-2162-3_65, 2012.
Lucchi, R. G., Camerlenghi, A., Rebesco, M., Colmenero-Hidalgo, E., Sierro,
F. J., Sagnotti, L., and Caburlotto, A.: Postglacial sedimentary processes
on the Storfjorden and Kveithola trough mouth fans: Significance of extreme
glacimarine sedimentation, Global Planet. Change, 111, 309–326,
https://doi.org/10.1016/j.gloplacha.2013.10.008, 2013.
Macías, J., Vázquez, J. T., Fernández-Salas, L. M.,
González-Vida, J. M., Bárcenas, P., Castro, M. J.,
Díaz-del-Río, V., and Alonso, B.: The Al-Borani submarine
landslide and associated tsunami, A modelling approach, Mar. Geol, 361,
79–95, https://doi.org/10.1016/j.margeo.2014.12.006, 2015.
Macías, J., Castro, M. J., Ortega, S., and González-Vida, J. M.: Performance assessment of Tsunami-HySEA model for NTHMP tsunami currents benchmarking, Field cases, Ocean Model., 152, 101645, https://doi.org/10.1016/j.ocemod.2020.101645, 2020.
Macías, J., Escalante, C., and Castro, M. J.: Multilayer-HySEA model validation for landslide-generated tsunamis – Part 1: Rigid slides, Nat. Hazards Earth Syst. Sci., 21, 775–789, https://doi.org/10.5194/nhess-21-775-2021, 2021.
Maslin, M., Mikkelsen, N., Vilela, C., and Haq, B.: Sea-level–and
gas-hydrate–controlled catastrophic sediment failures of the Amazon Fan,
Geology, 26, 1107–1110, https://doi.org/10.1130/0091-7613(1998)026<1107:SLAGHC>2.3.CO;2, 1998.
Meleshko, V. P., Golitsyn, G. S., Govorkova, V. A., Demchenko, P. F.,
Eliseev, A. V., Kattsov, V. M., and Sporyshev, P. V.: Anthropogenic climate
change in Russia in the 21st century: An ensemble of climate model
projections, Meteorologiya i gidrologiya, 4, 38–49, 2004.
Moernaut, J., Van Daele, M., Strasser, M., Clare, M. A., Heirman, K., Viel,
M., Cardenas, J., Kilian, R., Ladrón de Guevara, B., Pino, M., Urrutia,
R., and De Batist, M.: Lacustrine turbidites produced by surficial slope
sediment remobilization: A mechanism for continuous and sensitive turbidite
paleoseismic records, Mar. Geol, 384, 159–176,
https://doi.org/10.1016/j.margeo.2015.10.009, 2017.
Newton, A. M. and Huuse, M.: Glacial geomorphology of the central Barents
Sea: implications for the dynamic deglaciation of the Barents Sea Ice Sheet,
Mar. Geol, 387, 114–131, https://doi.org/10.1016/j.margeo.2017.04.001, 2017.
Ottesen, D., Dowdeswell, J. A., and Rise, S.: Submarine landforms and the
reconstruction of fast-flowing ice streams within a large Quaternary ice
sheet: The 2500-km-long Norwegian-Svalbard margin (57∘–80∘ N), Geol. Soc. Am. Bull., 117, 1033–1050, https://doi.org/10.1130/B25577.1, 2005.
Pedrosa, M. T., Camerlenghi, A., De Mol, B., Urgeles, R., Rebesco, M., and
Lucchi, R. G.: Seabed morphology and shallow sedimentary structure of the
Storfjorden and Kveithola trough-mouth fans (North West Barents Sea), Mar.
Geol., 286, 65–81, https://doi.org/10.1016/j.margeo.2011.05.009, 2011.
Piper, D. J., Cochonat, P., and Morrison, M. L.: The sequence of events
around the epicentre of the 1929 Grand Banks earthquake: initiation of
debris flows and turbidity current inferred from sidescan sonar,
Sedimentology, 46, 79–97, https://doi.org/10.1046/j.1365-3091.1999.00204.x, 1999.
Pirli, M., Schweitzer, J., and Paulsen, B.: The Storfjorden, Svalbard,
2008–2012 aftershock sequence: Seismotectonics in a polar environment,
Tectonophysics, 601, 192–205, https://doi.org/10.1016/j.tecto.2013.05.010, 2013.
Pouliquen, O. and Forterre, Y.: Friction law for dense granular flows:
application to the motion of a mass down a rough inclined plane, J.
Fluid Mech., 453, 133–151, https://doi.org/10.1017/S0022112001006796, 2002.
Pudasaini, S. P.: Dynamics of submarine debris flow and tsunami, Acta
Mech., 225, 2423–2434, https://doi.org/10.1007/s00707-014-1126-0, 2014.
Ramadan, K. T.: Near- and far-field tsunami waves, displaced water volume, potential energy and velocity flow rates by a stochastic submarine earthquake source model, Nat. Hazards Earth Syst. Sci. Discuss. [preprint], https://doi.org/10.5194/nhess-2018-107, 2018.
Rebesco, M., Pedrosa, M. T., Camerlenghi, A., Lucchi, R. G., Sauli, C., De
Mol, B., Madrussani, G., Urgeles, R., Rossi, G., and Böhm, G.: One
million years of climatic generated landslide events on the northwestern
Barents Sea continental margin, in:
Submarine Mass Movements and Their Consequences. Advances in Natural and
Technological Hazards Research, edited by: Yamada, Y., Kawamura, K., Ikehara, K.,
Ogawa, Y., Urgeles, R., Mosher, D., Chaytor, J., and Strasser, M., 31, Springer, Dordrecht, the Netherlands,
747–756, https://doi.org/10.1007/978-94-007-2162-3_66, 2012.
Rebesco, M., Laberg, J. S., Pedrosa, M. T., Camerlenghi, A., Lucchi, R. G., Zgur, F., and Wardell, N.: Onset and growth of trough-mouth fans on the north-western Barents Sea margin–implications for the evolution of the Barents Sea/Svalbard ice sheet, Quaternary Sci. Rev., 92, 227–234, https://doi.org/10.1016/j.quascirev.2013.08.015, 2014.
Rodríguez-Morata, C., Villacorta, S., Stoffel, M., and
Ballesteros-Cánovas, J. A.: Assessing strategies to mitigate debris-flow
risk in Abancay province, south-central Peruvian Andes, Geomorphology, 342,
127–139, https://doi.org/10.1016/j.geomorph.2019.06.012, 2019.
Salaree, A. and Okal, E.: Effects of bathymetry complexity on tsunami
propagation: a spherical harmonics approach, Geophys. J.
Int., 223, 632–647, https://doi.org/10.1093/gji/ggaa334, 2020.
Sejrup, H. P., Hjelstuen, B. O., Torbjørn Dahlgren, K. I., Haflidason, H., Kuijpers, A., Nygård, A., Praeg, D., and Vorren, T. O.: Pleistocene glacial history of the NW European continental margin,
Mar. Petrol. Geol.,
22, 1111–1129, https://doi.org/10.1016/j.marpetgeo.2004.09.007, 2005.
Sierro, F. J., Andersen, N., Bassetti, M. A., Berné, S., Canals, M.,
Curtis, J. H., Dennielou, B., Flores, J. A., Frigola, J., Gonzalez-Mora, B.,
Grimalt, J. O., Hodell, D. A., Jouet, G., Pérez-Folgado, M., and
Schneider, R.: Phase relationship between sea level and abrupt climate
change, Quaterny Sci. Rev., 28, 2867–2881, https://doi.org/10.1016/j.quascirev.2009.07.019, 2009.
Skogseth, R., Olivier, L. L., Nilsen, F., Falck, E., Fraser, N., Tverberg,
V., and Falk-Petersen, S.: Variability and decadal trends in the Isfjorden
(Svalbard) ocean climate and circulation – An indicator for climate change in
the European Arctic, Prog. Oceanogr., 187, 102394,
https://doi.org/10.1016/j.pocean.2020.102394, 2020.
Solheim, A., Berg, K., Forsberg, C. F., and Bryn, P.: The Storegga Slide
complex: repetitive large scale sliding with similar cause and development,
Mar. Petrol. Geol., 22, 97–107,
doi.org:10.1016/j.marpetgeo.2004.10.013, 2005.
Sun, Q. and Leslie, S.: Tsunamigenic potential of an incipient submarine
slope failure in the northern South China Sea, Mar. Petrol. Geol., 112, 104111,
https://doi.org/10.1016/j.marpetgeo.2019.104111, 2020.
Synolakis, C. E., Yalciner, A. C., Borrero, J. C., and Plafker, G.: Modeling of the November 3, 1994 Skagway, Alaska tsunami, in: Solution to Coastal Disasters Conference, San Diego, California, United States, 24–27 February, 915–927, https://doi.org/10.1061/40605(258)78, 2002.
Tappin, D. R.: Submarine mass failures as tsunami sources: their climate
control, Philos. T. R. Soc. A, 368, 2417–2434,
https://doi.org/10.1098/rsta.2010.0079, 2010.
Thomson, R. E., Rabinovich, A. B., Kulikov, E. A., Fine, I. V., and
Bornhold, B. D.: On numerical simulation of the landslide-generated tsunami
of November 3, 1994 in Skagway Harbor, Alaska, in: Tsunami research at the
end of a critical decade, Springer, Dordrecht, 243–282, https://doi.org/10.1007/978-94-017-3618-3_17, 2001.
Tinti, S., Bortolucci, E., and Romagnoli, C.: Computer simulations of
tsunamis due to sector collapse at Stromboli, Italy, J. Volcanol.
Geoth. Res., 96, 103–128, https://doi.org/10.1016/S0377-0273(99)00138-9, 2000.
Urgeles, R., Bahk, J. J., Lee, S. H., Horozal, S., Cukur, D., Kim, S. P., and Um, I. K.: Tsunami hazard from submarine landslides: scenario-based assessment in the Ulleung Basin, East Sea (Japan Sea), Geosci. J., 23, 439–460, https://doi.org/10.1007/s12303-018-0044-x, 2019.
Urlaub, M., Talling, P. J., and Masson, D. G.: Timing and frequency of large
submarine landslides: implications for understanding triggers and future
geohazard, Quaterny Sci. Rev., 72, 63–82, https://doi.org/10.1016/j.quascirev.2013.04.020,
2013.
Vanneste, M., Mienert, J., and Bünz, S.: The Hinlopen Slide: a giant,
submarine slope failure on the northern Svalbard margin, Arctic Ocean, Earth
Planet. Sc. Lett., 245, 373–388, https://doi.org/10.1016/j.epsl.2006.02.045,
2006.
Vanneste, M., Sultan, N., Garziglia, S., Forsberg, C. F., and L'Heureux, J.
S.: Seafloor instabilities and sediment deformation processes: The need for
integrated, multi-disciplinary investigations, Mar. Geol., 352, 183–214,
https://doi.org/10.1016/j.margeo.2014.01.005, 2014.
Vázquez, J. T., Ercilla, G., Alonso, B., Peláez, J. A., Palomino,
D., León, R., Barcenas, P., Casas, D., Estrada, F., Fernández-Puga, M. C., Galindo-Zaldívar, J., Henares, J., Llorente, M., Sánchez-Guillamón, O., d'Acremont, E., Ammar, A., Chourak, M., Fernández-Salas, L. M., López-González, N., and Lafuerza, S.: Triggering Mechanisms of
Tsunamis in the Gulf of Cadiz and the Alboran Sea: An Overview, in:
Historical Earthquakes, Tsunamis and Archaeology in the Iberian Peninsula
(Natural Science in Archaeology), edited by: Álvarez-Martí-Aguilar,
M., and Prieto, F. M., Springer, Singapore, 65–104,
https://doi.org/10.1007/978-981-19-1979-4_4, 2022.
Winkelmann, D., Geissler, W., Schneider, J., and Stein, R.: Dynamics and
timing of the Hinlopen/Yermak Megaslide north of Spitsbergen, Arctic Ocean,
Mar. Geol,, 250, 34–50, https://doi.org/10.1016/j.margeo.2007.11.013, 2008.
Worsley, D., Aga, O. J., Dalland, A., Elverhøi, A., and Thon, A.: The
Geological History of Svalbard, Evolution of an Arctic Archipelago, Statoil,
Asker Trykkeri, Stavanger, 121, 1986.
Zhang, W., Almgren, A., Beckner, V., Bell, J., Blaschke, J., Chan, C., and
Zingale, M.: AMReX: a framework for block-structured adaptive mesh
refinement, J. Open Source Softw., 4, 1370–1370, https://doi.org/10.21105/joss.01370, 2019.
Short summary
The L-ML-HySEA (Landslide Multilayer Hyperbolic Systems and Efficient Algorithms) model of the tsunami triggered by the Storfjorden LS-1 landslide provides new insights into the sliding mechanism and bathymetry controlling the propagation, amplitude values and shoaling effects as well as coastal impact times. This case study provides new perspectives on tsunami hazard assessment in polar margins, where global climatic change and its related ocean warming may contribute to landslide trigger.
The L-ML-HySEA (Landslide Multilayer Hyperbolic Systems and Efficient Algorithms) model of the...
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