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Tsunamis from source to coast

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Resumo:Tsunami disasters pose a significant threat to coastal communities. In the last decades, tsunamis caused enormous destruction and exceeding 250000 fatalities. International efforts led to sig-nificant advances in tsunami science and research, but recent events demonstrated some limi-tations. Thus, it is essential to increase our knowledge of the source to coast tsunami phenom-enon. A better understanding of potential tectonic structures and other generation mechanisms is needed, especially in complex geologic domains or where sources are unknown. Furthermore, we need to improve Tsunami Warning Systems (TWSs) to provide timely alerts for communi-ties in the near field. Therefore, potential tsunamigenic sources in the diffuse plate boundary setting and the near field of the southwest Iberian margin (SWIM) are investigated. For the March 31, 1761, trans-atlantic tsunami, numerical modelling has been used to propose a structure that agrees with tsunami travel times, tsunami observations, macroseismic data, and kinematic plate modelling. Since there exists a description of a tsunami for the November 11, 1858, Sétubal earthquake, its source has been investigated using macroseismic analysis. The analysis suggests a local structure in a compressive regime with weak to moderate tsunamigenic potential. Future tsu-nami hazard assessments need to include the sources of the investigated events. To quickly estimate the tsunami impact, the Tsunami Runup Predictor (TRP), an empirical source-to-coast method to instantly provide first-order estimates of the tsunami runup based on waveform parameters has been developed. The TRP is helpful for emergency managers and evacuation planning for near-field events. Moreover, the author of this thesis contributed to the tsunami impact assessment of September 28, 2018, Palu tsunami, where tsunamis generated by multiple sources caused runup heights up to 9.2 m. However, for local sources, tsunami warning remains challenging; thus, communities need to be prepared how to respond appropriately to earthquakes and tsunamis with or without warning.
Autores principais:Wronna, Martin
Assunto:Caracterização de perigo de tsunami Sistemas de alerta de tsunami Cálculo analítico de tsunami runup Modelo de equações de águas pouco profundas não-lineares Estimativas rápidas do tsunami runup Tsunami hazard Tsunami early warning systems Analytical runup computation Analytical runup computation Rapid tsunami runup estimation
Ano:2022
País:Portugal
Tipo de documento:tese de doutoramento
Tipo de acesso:acesso aberto
Instituição associada:Universidade de Lisboa
Idioma:inglês
Origem:Repositório da Universidade de Lisboa
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author Wronna, Martin
author_facet Wronna, Martin
author_role author
contributor_name_str_mv Baptista, Maria Ana
Kânoğlu, Utku
Repositório Científico de Acesso Aberto da ULisboa
country_str PT
creators_json_txt [{\"Person.name\":\"Wronna, Martin\",\"Person.identifier.orcid\":\"0000-0002-8773-3738\"}]
datacite.contributors.contributor.contributorName.fl_str_mv Baptista, Maria Ana
Kânoğlu, Utku
Repositório Científico de Acesso Aberto da ULisboa
datacite.creators.creator.creatorName.fl_str_mv Wronna, Martin
datacite.date.Accepted.fl_str_mv 2022-02-01T00:00:00Z
datacite.date.available.fl_str_mv 2022-07-06T11:39:02Z
datacite.date.embargoed.fl_str_mv 2022-07-06T11:39:02Z
datacite.rights.fl_str_mv http://purl.org/coar/access_right/c_abf2
datacite.subjects.subject.fl_str_mv Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
datacite.titles.title.fl_str_mv Tsunamis from source to coast
dc.contributor.none.fl_str_mv Baptista, Maria Ana
Kânoğlu, Utku
Repositório Científico de Acesso Aberto da ULisboa
dc.creator.none.fl_str_mv Wronna, Martin
dc.date.Accepted.fl_str_mv 2022-02-01T00:00:00Z
dc.date.available.fl_str_mv 2022-07-06T11:39:02Z
dc.date.embargoed.fl_str_mv 2022-07-06T11:39:02Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv http://hdl.handle.net/10451/53691
dc.language.none.fl_str_mv eng
dc.rights.none.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.subject.none.fl_str_mv Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
dc.title.fl_str_mv Tsunamis from source to coast
dc.type.none.fl_str_mv http://purl.org/coar/resource_type/c_db06
description Tsunami disasters pose a significant threat to coastal communities. In the last decades, tsunamis caused enormous destruction and exceeding 250000 fatalities. International efforts led to sig-nificant advances in tsunami science and research, but recent events demonstrated some limi-tations. Thus, it is essential to increase our knowledge of the source to coast tsunami phenom-enon. A better understanding of potential tectonic structures and other generation mechanisms is needed, especially in complex geologic domains or where sources are unknown. Furthermore, we need to improve Tsunami Warning Systems (TWSs) to provide timely alerts for communi-ties in the near field. Therefore, potential tsunamigenic sources in the diffuse plate boundary setting and the near field of the southwest Iberian margin (SWIM) are investigated. For the March 31, 1761, trans-atlantic tsunami, numerical modelling has been used to propose a structure that agrees with tsunami travel times, tsunami observations, macroseismic data, and kinematic plate modelling. Since there exists a description of a tsunami for the November 11, 1858, Sétubal earthquake, its source has been investigated using macroseismic analysis. The analysis suggests a local structure in a compressive regime with weak to moderate tsunamigenic potential. Future tsu-nami hazard assessments need to include the sources of the investigated events. To quickly estimate the tsunami impact, the Tsunami Runup Predictor (TRP), an empirical source-to-coast method to instantly provide first-order estimates of the tsunami runup based on waveform parameters has been developed. The TRP is helpful for emergency managers and evacuation planning for near-field events. Moreover, the author of this thesis contributed to the tsunami impact assessment of September 28, 2018, Palu tsunami, where tsunamis generated by multiple sources caused runup heights up to 9.2 m. However, for local sources, tsunami warning remains challenging; thus, communities need to be prepared how to respond appropriately to earthquakes and tsunamis with or without warning.
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funding.funder.identifier_str_mv http://doi.org/10.13039/501100001871
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funding.funder.name_str_mv Fundação para a Ciência e a Tecnologia
Fundação para a Ciência e a Tecnologia
funding.name_str_mv 6817 - DCRRNI ID
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person_str_mv Wronna, Martin
Wronna, Martin
https://www.ciencia-id.pt/1F1B-8B58-38C4
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spelling engpt_PTTsunami disasters pose a significant threat to coastal communities. In the last decades, tsunamis caused enormous destruction and exceeding 250000 fatalities. International efforts led to sig-nificant advances in tsunami science and research, but recent events demonstrated some limi-tations. Thus, it is essential to increase our knowledge of the source to coast tsunami phenom-enon. A better understanding of potential tectonic structures and other generation mechanisms is needed, especially in complex geologic domains or where sources are unknown. Furthermore, we need to improve Tsunami Warning Systems (TWSs) to provide timely alerts for communi-ties in the near field. Therefore, potential tsunamigenic sources in the diffuse plate boundary setting and the near field of the southwest Iberian margin (SWIM) are investigated. For the March 31, 1761, trans-atlantic tsunami, numerical modelling has been used to propose a structure that agrees with tsunami travel times, tsunami observations, macroseismic data, and kinematic plate modelling. Since there exists a description of a tsunami for the November 11, 1858, Sétubal earthquake, its source has been investigated using macroseismic analysis. The analysis suggests a local structure in a compressive regime with weak to moderate tsunamigenic potential. Future tsu-nami hazard assessments need to include the sources of the investigated events. To quickly estimate the tsunami impact, the Tsunami Runup Predictor (TRP), an empirical source-to-coast method to instantly provide first-order estimates of the tsunami runup based on waveform parameters has been developed. The TRP is helpful for emergency managers and evacuation planning for near-field events. Moreover, the author of this thesis contributed to the tsunami impact assessment of September 28, 2018, Palu tsunami, where tsunamis generated by multiple sources caused runup heights up to 9.2 m. However, for local sources, tsunami warning remains challenging; thus, communities need to be prepared how to respond appropriately to earthquakes and tsunamis with or without warning.application/pdfpt_PTTsunamis from source to coastPersonalWronna, MartinDSpacehttp://dspace.org/items/1e644d19-9f33-4b51-80dc-d74ed3789097DSpacehttp://dspace.org/items/1e644d19-9f33-4b51-80dc-d74ed3789097WronnaMartinCiência IDhttps://www.ciencia-id.pt1F1B-8B58-38C4ORCIDhttp://orcid.org0000-0002-8773-3738Baptista, Maria AnaKânoğlu, UtkuHostingInstitutionOrganizationalRepositório Científico de Acesso Aberto da ULisboae-mailmailto:repositorio@reitoria.ulisboa.ptrepositorio@reitoria.ulisboa.ptURNurn:tid:1015795862022-07-06T11:39:02Z2022-022021-122022-02-01T00:00:00ZHandlehttp://hdl.handle.net/10451/53691http://purl.org/coar/access_right/c_abf2open accessCaracterização de perigo de tsunamiSistemas de alerta de tsunamiCálculo analítico de tsunami runupModelo de equações de águas pouco profundas não-linearesEstimativas rápidas do tsunami runupTsunami hazardTsunami early warning systemsAnalytical runup computationAnalytical runup computationRapid tsunami runup estimation18131981 bytesFundação para a Ciência e a TecnologiaInstituto Dom Luiz6817 - DCRRNI IDCrossref Funder IDhttp://doi.org/10.13039/501100001871Fundação para a Ciência e a TecnologiaTsunamis from source to coastCrossref Funder IDhttp://doi.org/10.13039/501100001871literaturehttp://purl.org/coar/resource_type/c_db06doctoral thesishttp://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://repositorio.ulisboa.pt/bitstreams/c62700f6-eb7d-4f9c-8c39-8fff1b02f5fe/download
spellingShingle Tsunamis from source to coast
Wronna, Martin
Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
status SINGLETON
subject.fl_str_mv Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
title Tsunamis from source to coast
title_full Tsunamis from source to coast
title_fullStr Tsunamis from source to coast
title_full_unstemmed Tsunamis from source to coast
title_short Tsunamis from source to coast
title_sort Tsunamis from source to coast
topic Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
topic_facet Caracterização de perigo de tsunami
Sistemas de alerta de tsunami
Cálculo analítico de tsunami runup
Modelo de equações de águas pouco profundas não-lineares
Estimativas rápidas do tsunami runup
Tsunami hazard
Tsunami early warning systems
Analytical runup computation
Analytical runup computation
Rapid tsunami runup estimation
url http://hdl.handle.net/10451/53691
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