Extremely Strong Winds and Weather Patterns over Arctic seas

Strong wind is the main cause of storm sea waves. In order to minimize risks and damages from this phenomenon in the future, precise projections of future climate conditions are necessary. Extremely high wind speed events in the 20th - 21st centuries over Arctic seas were investigated using ERA-Inte...

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Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Galina Surkova, Aleksey Krylov
Format: Article in Journal/Newspaper
Language:English
Published: Lomonosov Moscow State University 2019
Subjects:
geo
Online Access:https://doi.org/10.24057/2071-9388-2019-22
https://doaj.org/article/8c5edd27a6fd4c9e85272ac85517328d
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:8c5edd27a6fd4c9e85272ac85517328d 2023-05-15T14:51:55+02:00 Extremely Strong Winds and Weather Patterns over Arctic seas Galina Surkova Aleksey Krylov 2019-10-01 https://doi.org/10.24057/2071-9388-2019-22 https://doaj.org/article/8c5edd27a6fd4c9e85272ac85517328d en eng Lomonosov Moscow State University 2071-9388 2542-1565 doi:10.24057/2071-9388-2019-22 https://doaj.org/article/8c5edd27a6fd4c9e85272ac85517328d undefined Geography, Environment, Sustainability, Vol 12, Iss 3, Pp 34-42 (2019) wind speed extremes global warming arctic weather patterns oceanatmosphere interaction geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.24057/2071-9388-2019-22 2023-01-22T18:38:46Z Strong wind is the main cause of storm sea waves. In order to minimize risks and damages from this phenomenon in the future, precise projections of future climate conditions are necessary. Extremely high wind speed events in the 20th - 21st centuries over Arctic seas were investigated using ERA-Interim reanalysis data (1981-2010) and CMIP5 models ensemble (RCP8.5 scenario, 2005-2100). Two different approaches were applied to investigate extreme wind events. The first one is traditional and involves direct analysis of wind speed data. It was used for the entire area of the Arctic seas. The second approach is based on an assumption that local and mesoscale extreme weather events are connected with large-scale synoptic processes. As it was shown in previous studies for the Black, Caspian and Baltic seas, it is possible to make climate projection of sea storm waves indirectly, studying the heterogeneity of sea level atmospheric pressure (SLP) fields that are the main factors of strong wind speed and wind waves. In this case, it is not necessary to run long-term simulations with a sea wave model to predict storm activity for the future climate. It is possible to analyze projections of storm SLP fields that are predicted by climate models much better than the wind speed required for a wave model. This method was implemented for the high wind speed events over the Barents Sea. Four major types of SLP fields accompanying high wind speed were revealed for the modern climate. It was shown that the frequency of their occurrence is expected to increase by the end of the 21st century. Article in Journal/Newspaper Arctic Barents Sea Global warming Unknown Arctic Barents Sea GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 12 3 34 42
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic wind speed extremes
global warming
arctic
weather patterns
oceanatmosphere interaction
geo
envir
spellingShingle wind speed extremes
global warming
arctic
weather patterns
oceanatmosphere interaction
geo
envir
Galina Surkova
Aleksey Krylov
Extremely Strong Winds and Weather Patterns over Arctic seas
topic_facet wind speed extremes
global warming
arctic
weather patterns
oceanatmosphere interaction
geo
envir
description Strong wind is the main cause of storm sea waves. In order to minimize risks and damages from this phenomenon in the future, precise projections of future climate conditions are necessary. Extremely high wind speed events in the 20th - 21st centuries over Arctic seas were investigated using ERA-Interim reanalysis data (1981-2010) and CMIP5 models ensemble (RCP8.5 scenario, 2005-2100). Two different approaches were applied to investigate extreme wind events. The first one is traditional and involves direct analysis of wind speed data. It was used for the entire area of the Arctic seas. The second approach is based on an assumption that local and mesoscale extreme weather events are connected with large-scale synoptic processes. As it was shown in previous studies for the Black, Caspian and Baltic seas, it is possible to make climate projection of sea storm waves indirectly, studying the heterogeneity of sea level atmospheric pressure (SLP) fields that are the main factors of strong wind speed and wind waves. In this case, it is not necessary to run long-term simulations with a sea wave model to predict storm activity for the future climate. It is possible to analyze projections of storm SLP fields that are predicted by climate models much better than the wind speed required for a wave model. This method was implemented for the high wind speed events over the Barents Sea. Four major types of SLP fields accompanying high wind speed were revealed for the modern climate. It was shown that the frequency of their occurrence is expected to increase by the end of the 21st century.
format Article in Journal/Newspaper
author Galina Surkova
Aleksey Krylov
author_facet Galina Surkova
Aleksey Krylov
author_sort Galina Surkova
title Extremely Strong Winds and Weather Patterns over Arctic seas
title_short Extremely Strong Winds and Weather Patterns over Arctic seas
title_full Extremely Strong Winds and Weather Patterns over Arctic seas
title_fullStr Extremely Strong Winds and Weather Patterns over Arctic seas
title_full_unstemmed Extremely Strong Winds and Weather Patterns over Arctic seas
title_sort extremely strong winds and weather patterns over arctic seas
publisher Lomonosov Moscow State University
publishDate 2019
url https://doi.org/10.24057/2071-9388-2019-22
https://doaj.org/article/8c5edd27a6fd4c9e85272ac85517328d
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Arctic
Barents Sea
Global warming
genre_facet Arctic
Barents Sea
Global warming
op_source Geography, Environment, Sustainability, Vol 12, Iss 3, Pp 34-42 (2019)
op_relation 2071-9388
2542-1565
doi:10.24057/2071-9388-2019-22
https://doaj.org/article/8c5edd27a6fd4c9e85272ac85517328d
op_rights undefined
op_doi https://doi.org/10.24057/2071-9388-2019-22
container_title GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
container_volume 12
container_issue 3
container_start_page 34
op_container_end_page 42
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