On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations

In the previous companion study, satellite data were used to describe peculiar characteristics of ocean surface wave fields, generated by two extra-tropical cyclones (ETCs) rapidly propagating in the North Atlantic. Based on a 2D parametric wave model, further details are now provided to analyse and...

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Published in:Remote Sensing
Main Authors: Vahid Cheshm Siyahi, Vladimir Kudryavtsev, Maria Yurovskaya, Fabrice Collard, Bertrand Chapron
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15092377
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/9/2377/ 2023-08-20T04:08:16+02:00 On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations Vahid Cheshm Siyahi Vladimir Kudryavtsev Maria Yurovskaya Fabrice Collard Bertrand Chapron agris 2023-04-30 application/pdf https://doi.org/10.3390/rs15092377 EN eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs15092377 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 9; Pages: 2377 extreme waves extra-tropical cyclones altimeter CFOSAT-SWIM ocean surface waves remote sensing Atlantic ocean ocean surface waves monitoring and modeling parametric-2D wave-ray model swell evolution synthetic aperture radar Text 2023 ftmdpi https://doi.org/10.3390/rs15092377 2023-08-01T09:55:21Z In the previous companion study, satellite data were used to describe peculiar characteristics of ocean surface wave fields, generated by two extra-tropical cyclones (ETCs) rapidly propagating in the North Atlantic. Based on a 2D parametric wave model, further details are now provided to analyse and interpret the spatio-temporal evolution of very intense ETC-generated waves. Significant wave height and wavelength values are shown to reach extreme values, 18 m and 500 m, respectively. Resulting energetic swell systems waves then radiate in the whole eastern part of the North Atlantic, and more particularly in the Norwegian sea region. Moving to higher latitudes, wind forcing characteristics of ETCs evolve, with the shape of the wind field changing from quasi-cyclonic to “air jets/Icelandic lows”. In this paper, the resulting swell generation and propagation, after the deformation of an individual ETC, were studied, as well. Confirmed with comparisons with multi-satellite observations, the application of the parametric-2D wave-ray model was demonstrated to provide robust and highly detailed information on wave generation under very complex wind regime changes. Text North Atlantic Norwegian Sea MDPI Open Access Publishing Norwegian Sea Remote Sensing 15 9 2377
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic extreme waves
extra-tropical cyclones
altimeter
CFOSAT-SWIM
ocean surface waves remote sensing
Atlantic ocean
ocean surface waves monitoring and modeling
parametric-2D wave-ray model
swell evolution
synthetic aperture radar
spellingShingle extreme waves
extra-tropical cyclones
altimeter
CFOSAT-SWIM
ocean surface waves remote sensing
Atlantic ocean
ocean surface waves monitoring and modeling
parametric-2D wave-ray model
swell evolution
synthetic aperture radar
Vahid Cheshm Siyahi
Vladimir Kudryavtsev
Maria Yurovskaya
Fabrice Collard
Bertrand Chapron
On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
topic_facet extreme waves
extra-tropical cyclones
altimeter
CFOSAT-SWIM
ocean surface waves remote sensing
Atlantic ocean
ocean surface waves monitoring and modeling
parametric-2D wave-ray model
swell evolution
synthetic aperture radar
description In the previous companion study, satellite data were used to describe peculiar characteristics of ocean surface wave fields, generated by two extra-tropical cyclones (ETCs) rapidly propagating in the North Atlantic. Based on a 2D parametric wave model, further details are now provided to analyse and interpret the spatio-temporal evolution of very intense ETC-generated waves. Significant wave height and wavelength values are shown to reach extreme values, 18 m and 500 m, respectively. Resulting energetic swell systems waves then radiate in the whole eastern part of the North Atlantic, and more particularly in the Norwegian sea region. Moving to higher latitudes, wind forcing characteristics of ETCs evolve, with the shape of the wind field changing from quasi-cyclonic to “air jets/Icelandic lows”. In this paper, the resulting swell generation and propagation, after the deformation of an individual ETC, were studied, as well. Confirmed with comparisons with multi-satellite observations, the application of the parametric-2D wave-ray model was demonstrated to provide robust and highly detailed information on wave generation under very complex wind regime changes.
format Text
author Vahid Cheshm Siyahi
Vladimir Kudryavtsev
Maria Yurovskaya
Fabrice Collard
Bertrand Chapron
author_facet Vahid Cheshm Siyahi
Vladimir Kudryavtsev
Maria Yurovskaya
Fabrice Collard
Bertrand Chapron
author_sort Vahid Cheshm Siyahi
title On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
title_short On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
title_full On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
title_fullStr On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
title_full_unstemmed On Surface Waves Generated by Extra-Tropical Cyclones—Part II: Simulations
title_sort on surface waves generated by extra-tropical cyclones—part ii: simulations
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15092377
op_coverage agris
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre North Atlantic
Norwegian Sea
genre_facet North Atlantic
Norwegian Sea
op_source Remote Sensing; Volume 15; Issue 9; Pages: 2377
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs15092377
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15092377
container_title Remote Sensing
container_volume 15
container_issue 9
container_start_page 2377
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