Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands)
Special issue Tsunamis: from source processes to coastal hazard and warning.-- 20 pages, 9 figures, 2 tables, video supplement https://doi.org/10.5446/56981 and https://doi.org/10.5446/5698.-- Code and data availability: The SVAIS data are hosted by the Oceanography Cruise and Data Catalogue of CSIC-UTM/Marine Technology Unit https://doi.org/10.20351/29HE20070802 (CSIC, 2018)
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European Geosciences Union
2022-11
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dig-icm-es-10261-2846642022-12-13T02:10:03Z Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) Pedrosa-González, María Teresa González-Vida, José Manuel Galindo Zaldívar, Jesús Ortega-Acosta, Sergio Castro, Manuel Jesús Casas, David Ercilla, Gemma Junta de Andalucía Agencia Estatal de Investigación (España) Ministerio de Ciencia, Innovación y Universidades (España) CSIC - Unidad de Recursos de Información Científica para la Investigación (URICI) Special issue Tsunamis: from source processes to coastal hazard and warning.-- 20 pages, 9 figures, 2 tables, video supplement https://doi.org/10.5446/56981 and https://doi.org/10.5446/5698.-- Code and data availability: The SVAIS data are hosted by the Oceanography Cruise and Data Catalogue of CSIC-UTM/Marine Technology Unit https://doi.org/10.20351/29HE20070802 (CSIC, 2018) A modelling approach to understand the tsunamigenic potentiality of submarine landslides will provide new perspectives on tsunami hazard threat, mostly in polar margins where global climatic change and its related ocean warming may induce future landslides. Here, we use the L-ML-HySEA (Landslide Multilayer Hyperbolic Systems and Efficient Algorithms) numerical model, including wave dispersion, to provide new insights into factors controlling the tsunami characteristics triggered by the Storfjorden LS-1 landslide (southwestern Svalbard). Tsunami waves, determined mainly by the sliding mechanism and the bathymetry, consist of two initial wave dipoles, with troughs to the northeast (Spitsbergen and towards the continent) and crests to the south (seawards) and southwest (Bear Island), reaching more than 3 m of amplitude above the landslide and finally merging into a single wave dipole. The tsunami wave propagation and its coastal impact are governed by the Storfjorden and Kveithola glacial troughs and by the bordering Spitsbergen Bank, which shape the continental shelf. This local bathymetry controls the direction of propagation with a crescent shape front, in plan view, and is responsible for shoaling effects of amplitude values (4.2 m in trough to 4.3 m in crest), amplification (3.7 m in trough to 4 m in crest) and diffraction of the tsunami waves, as well as influencing their coastal impact times This research has been supported by the Consejería de Universidad, Investigación e Innovación, Junta de Andalucía (grant nos. B-RNM-301-UGR18, P18-RT-3275 and RNM 148; University of Granada, FEDER) and the Agencia Estatal de Investigacíon (grant nos. PID2019-108880RJ-I00/AEI/10.13039/501100011033, POL2006-07390/CGL and CTM2009-06370-E/ANT). We acknowledge support of the publication fee by the CSIC Open Access Publication Support Initiative through its Unit of Information Resources for Research (URICI) With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S) Peer reviewed 2022-12-12T12:36:11Z 2022-12-12T12:36:11Z 2022-11 artículo Natural Hazards and Earth System Sciences 22(12): 3839-3858 (2022) 1561-8633 CEX2019-000928-S http://hdl.handle.net/10261/284664 10.5194/nhess-22-3839-2022 1684-9981 http://dx.doi.org/10.13039/501100011033 http://dx.doi.org/10.13039/501100011011 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2019-108880RJ-I00/ES/ANISOTROPIA ELECTRICA DEL MANTO EN LA ANTARTIDA, NUEVA PERSPECTIVA PARA EL ANALISIS DEL AJUSTE ISOSTATICO GLACIAL Y LOS CAMBIOS EN EL NIVEL DEL MAR/ Publisher's version https://doi.org/10.5194/nhess-22-3839-2022 Sí open European Geosciences Union |
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Special issue Tsunamis: from source processes to coastal hazard and warning.-- 20 pages, 9 figures, 2 tables, video supplement https://doi.org/10.5446/56981 and https://doi.org/10.5446/5698.-- Code and data availability: The SVAIS data are hosted by the Oceanography Cruise and Data Catalogue of CSIC-UTM/Marine Technology Unit https://doi.org/10.20351/29HE20070802 (CSIC, 2018) |
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Junta de Andalucía |
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Junta de Andalucía Pedrosa-González, María Teresa González-Vida, José Manuel Galindo Zaldívar, Jesús Ortega-Acosta, Sergio Castro, Manuel Jesús Casas, David Ercilla, Gemma |
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Pedrosa-González, María Teresa González-Vida, José Manuel Galindo Zaldívar, Jesús Ortega-Acosta, Sergio Castro, Manuel Jesús Casas, David Ercilla, Gemma |
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Pedrosa-González, María Teresa González-Vida, José Manuel Galindo Zaldívar, Jesús Ortega-Acosta, Sergio Castro, Manuel Jesús Casas, David Ercilla, Gemma Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
author_sort |
Pedrosa-González, María Teresa |
title |
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
title_short |
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
title_full |
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
title_fullStr |
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
title_full_unstemmed |
Simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of Storfjorden LS-1 (southwestern Svalbard Islands) |
title_sort |
simulation of tsunami induced by a submarine landslide in a glaciomarine margin: the case of storfjorden ls-1 (southwestern svalbard islands) |
publisher |
European Geosciences Union |
publishDate |
2022-11 |
url |
http://hdl.handle.net/10261/284664 http://dx.doi.org/10.13039/501100011033 http://dx.doi.org/10.13039/501100011011 |
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