Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula

ABSTRACT. This paper assesses the evolution of storminess along the northern coast of the Iberian Peninsula through the calculation of extreme (1%) Total Water Levels (eTWL) on both observed (tide gauge and buoy data) and hindcasted (SIMAR-44) data. Those events were first identified and then charac...

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Main Authors: Rasilla, Domingo Fernando, García Codrón, Juan Carlos
Other Authors: Universidad de Cantabria
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:http://hdl.handle.net/10902/3426
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spelling ftunivcantabria:oai:repositorio.unican.es:10902/3426 2023-05-15T17:34:03+02:00 Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula Rasilla, Domingo Fernando García Codrón, Juan Carlos Universidad de Cantabria 2011-02-23 http://hdl.handle.net/10902/3426 eng eng Copernicus Publications 1561-8633 http://hdl.handle.net/10902/3426 Atribución 3.0 España http://creativecommons.org/licenses/by/3.0/es/ openAccess CC-BY Natural Hazards and Earth System Sciences, 2011, 11, 613-625 info:eu-repo/semantics/article publishedVersion 2011 ftunivcantabria 2023-02-20T10:28:30Z ABSTRACT. This paper assesses the evolution of storminess along the northern coast of the Iberian Peninsula through the calculation of extreme (1%) Total Water Levels (eTWL) on both observed (tide gauge and buoy data) and hindcasted (SIMAR-44) data. Those events were first identified and then characterized in terms of oceanographic parameters and atmospheric circulation features. Additionally, an analysis of the long-term trends in both types of data was performed. Most of the events correspond to a rough wave climate and moderate storm surges, linked to extratropical disturbances following a northern track. While local atmospheric conditions seem to be evolving towards lesser storminess, their impact has been balanced by the favorable exposure of the northern coast of the Iberian Peninsula to the increasing frequency and strength of distant disturbances crossing the North Atlantic. This evolution is also correctly reproduced by the simulated long-term evolution of the forcing component (meteorological sea level residuals and wave run up) of the Total Water Level values calculated from the SIMAR 44 database, since sea level residuals have been experiencing a reduction while waves are arriving with longer periods. Finally, the addition of the rate of relative sea level trend to the temporal evolution of the atmospheric forcing component of the Total Water Level values is enough to simulate more frequent and persistent eTWL. Article in Journal/Newspaper North Atlantic Universidad de Cantabria: UCrea
institution Open Polar
collection Universidad de Cantabria: UCrea
op_collection_id ftunivcantabria
language English
description ABSTRACT. This paper assesses the evolution of storminess along the northern coast of the Iberian Peninsula through the calculation of extreme (1%) Total Water Levels (eTWL) on both observed (tide gauge and buoy data) and hindcasted (SIMAR-44) data. Those events were first identified and then characterized in terms of oceanographic parameters and atmospheric circulation features. Additionally, an analysis of the long-term trends in both types of data was performed. Most of the events correspond to a rough wave climate and moderate storm surges, linked to extratropical disturbances following a northern track. While local atmospheric conditions seem to be evolving towards lesser storminess, their impact has been balanced by the favorable exposure of the northern coast of the Iberian Peninsula to the increasing frequency and strength of distant disturbances crossing the North Atlantic. This evolution is also correctly reproduced by the simulated long-term evolution of the forcing component (meteorological sea level residuals and wave run up) of the Total Water Level values calculated from the SIMAR 44 database, since sea level residuals have been experiencing a reduction while waves are arriving with longer periods. Finally, the addition of the rate of relative sea level trend to the temporal evolution of the atmospheric forcing component of the Total Water Level values is enough to simulate more frequent and persistent eTWL.
author2 Universidad de Cantabria
format Article in Journal/Newspaper
author Rasilla, Domingo Fernando
García Codrón, Juan Carlos
spellingShingle Rasilla, Domingo Fernando
García Codrón, Juan Carlos
Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
author_facet Rasilla, Domingo Fernando
García Codrón, Juan Carlos
author_sort Rasilla, Domingo Fernando
title Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
title_short Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
title_full Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
title_fullStr Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
title_full_unstemmed Evolution of extreme Total Water Levels along the northern coast of the Iberian Peninsula
title_sort evolution of extreme total water levels along the northern coast of the iberian peninsula
publisher Copernicus Publications
publishDate 2011
url http://hdl.handle.net/10902/3426
genre North Atlantic
genre_facet North Atlantic
op_source Natural Hazards and Earth System Sciences, 2011, 11, 613-625
op_relation 1561-8633
http://hdl.handle.net/10902/3426
op_rights Atribución 3.0 España
http://creativecommons.org/licenses/by/3.0/es/
openAccess
op_rightsnorm CC-BY
_version_ 1766132748028739584