On Surface Waves in Arctic Seas

International audience Surface waves in the Arctic Seas are jointly analyzed using satellite altimeter observations, classical fetch and duration laws of wave development, and a two-dimensional parametric wave model. A simplified scenario is first considered for the wave development under known phys...

Full description

Bibliographic Details
Published in:Boundary-Layer Meteorology
Main Authors: Kudryavtsev, Vladimir, Cheshm Siyahi, Vahid, Yurovskaya, Maria, Chapron, Bertrand
Other Authors: Laboratoire d'Océanographie Physique et Spatiale (LOPS), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://hal.science/hal-04203944
https://doi.org/10.1007/s10546-022-00768-9
id ftunivbrest:oai:HAL:hal-04203944v1
record_format openpolar
spelling ftunivbrest:oai:HAL:hal-04203944v1 2024-04-14T08:07:02+00:00 On Surface Waves in Arctic Seas Kudryavtsev, Vladimir Cheshm Siyahi, Vahid Yurovskaya, Maria Chapron, Bertrand Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2023-05 https://hal.science/hal-04203944 https://doi.org/10.1007/s10546-022-00768-9 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-022-00768-9 hal-04203944 https://hal.science/hal-04203944 doi:10.1007/s10546-022-00768-9 ISSN: 0006-8314 EISSN: 1573-1472 Boundary-Layer Meteorology https://hal.science/hal-04203944 Boundary-Layer Meteorology, 2023, 187, pp.267-294. ⟨10.1007/s10546-022-00768-9⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2023 ftunivbrest https://doi.org/10.1007/s10546-022-00768-9 2024-03-21T16:22:40Z International audience Surface waves in the Arctic Seas are jointly analyzed using satellite altimeter observations, classical fetch and duration laws of wave development, and a two-dimensional parametric wave model. A simplified scenario is first considered for the wave development under known physical fetch conditions during cold air outbreak events. Wave developments are found to agree well with the fetch laws, given known wave fetch and fetch-averaged wind speed, for significant wave heights (SWHs) less than 4–6 m and wind speeds below 20 m s−1. Wind wave conditions remarkably change for moving storms, associated with rapidly evolving polar lows (PLs). For such conditions, wind-generated waves exhibit properties similar to those encountered during tropical cyclones (TCs), reaching very large SWHs (8–12 m) and long wavelengths (up to 350 m). Still, wave parametrizations based on the extended fetch concept, previously developed for TC conditions, cannot be directly applied to PL cases due to their inherent marked space–time non-stationarity. Instead, an extended duration concept for wave development under PLs is suggested. Extended duration laws provide first-guess wave parameters, based on characteristic wind speed, translation velocity, spatial scale, and duration of a PL. A 2D parametric wave model, previously developed for TC conditions, is then applied to simulate waves generated during cold air outbreaks and PLs. Comparisons with altimeter measurements are favourable making it possible to consider this simple modelling tool for fast estimates and predictions of waves generated under highly variable Arctic wind conditions. Article in Journal/Newspaper Arctic Université de Bretagne Occidentale: HAL Arctic Boundary-Layer Meteorology 187 1-2 267 294
institution Open Polar
collection Université de Bretagne Occidentale: HAL
op_collection_id ftunivbrest
language English
topic [SDU]Sciences of the Universe [physics]
spellingShingle [SDU]Sciences of the Universe [physics]
Kudryavtsev, Vladimir
Cheshm Siyahi, Vahid
Yurovskaya, Maria
Chapron, Bertrand
On Surface Waves in Arctic Seas
topic_facet [SDU]Sciences of the Universe [physics]
description International audience Surface waves in the Arctic Seas are jointly analyzed using satellite altimeter observations, classical fetch and duration laws of wave development, and a two-dimensional parametric wave model. A simplified scenario is first considered for the wave development under known physical fetch conditions during cold air outbreak events. Wave developments are found to agree well with the fetch laws, given known wave fetch and fetch-averaged wind speed, for significant wave heights (SWHs) less than 4–6 m and wind speeds below 20 m s−1. Wind wave conditions remarkably change for moving storms, associated with rapidly evolving polar lows (PLs). For such conditions, wind-generated waves exhibit properties similar to those encountered during tropical cyclones (TCs), reaching very large SWHs (8–12 m) and long wavelengths (up to 350 m). Still, wave parametrizations based on the extended fetch concept, previously developed for TC conditions, cannot be directly applied to PL cases due to their inherent marked space–time non-stationarity. Instead, an extended duration concept for wave development under PLs is suggested. Extended duration laws provide first-guess wave parameters, based on characteristic wind speed, translation velocity, spatial scale, and duration of a PL. A 2D parametric wave model, previously developed for TC conditions, is then applied to simulate waves generated during cold air outbreaks and PLs. Comparisons with altimeter measurements are favourable making it possible to consider this simple modelling tool for fast estimates and predictions of waves generated under highly variable Arctic wind conditions.
author2 Laboratoire d'Océanographie Physique et Spatiale (LOPS)
Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Kudryavtsev, Vladimir
Cheshm Siyahi, Vahid
Yurovskaya, Maria
Chapron, Bertrand
author_facet Kudryavtsev, Vladimir
Cheshm Siyahi, Vahid
Yurovskaya, Maria
Chapron, Bertrand
author_sort Kudryavtsev, Vladimir
title On Surface Waves in Arctic Seas
title_short On Surface Waves in Arctic Seas
title_full On Surface Waves in Arctic Seas
title_fullStr On Surface Waves in Arctic Seas
title_full_unstemmed On Surface Waves in Arctic Seas
title_sort on surface waves in arctic seas
publisher HAL CCSD
publishDate 2023
url https://hal.science/hal-04203944
https://doi.org/10.1007/s10546-022-00768-9
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source ISSN: 0006-8314
EISSN: 1573-1472
Boundary-Layer Meteorology
https://hal.science/hal-04203944
Boundary-Layer Meteorology, 2023, 187, pp.267-294. ⟨10.1007/s10546-022-00768-9⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-022-00768-9
hal-04203944
https://hal.science/hal-04203944
doi:10.1007/s10546-022-00768-9
op_doi https://doi.org/10.1007/s10546-022-00768-9
container_title Boundary-Layer Meteorology
container_volume 187
container_issue 1-2
container_start_page 267
op_container_end_page 294
_version_ 1796304296137981952