Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia

The recurrence of extreme wind waves in the Kara Sea strongly influences the Arctic climate change. The period 2000–2010 is characterized by significant climate warming, a reduction of the sea ice in the Arctic. The main motivation of this research to assess the impact of climate change on storm act...

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Published in:Water
Main Authors: Stanislav Myslenkov, Vladimir Platonov, Alexander Kislov, Ksenia Silvestrova, Igor Medvedev
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/w13050648
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spelling ftmdpi:oai:mdpi.com:/2073-4441/13/5/648/ 2023-08-20T04:04:19+02:00 Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia Stanislav Myslenkov Vladimir Platonov Alexander Kislov Ksenia Silvestrova Igor Medvedev agris 2021-02-28 application/pdf https://doi.org/10.3390/w13050648 EN eng Multidisciplinary Digital Publishing Institute Oceans and Coastal Zones https://dx.doi.org/10.3390/w13050648 https://creativecommons.org/licenses/by/4.0/ Water; Volume 13; Issue 5; Pages: 648 the Kara Sea wave climate storm activity wind waves wave modeling WAVEWATCH III probabilistic analysis extreme waves Text 2021 ftmdpi https://doi.org/10.3390/w13050648 2023-08-01T01:10:10Z The recurrence of extreme wind waves in the Kara Sea strongly influences the Arctic climate change. The period 2000–2010 is characterized by significant climate warming, a reduction of the sea ice in the Arctic. The main motivation of this research to assess the impact of climate change on storm activity over the past 39 years in the Kara Sea. The paper presents the analysis of wave climate and storm activity in the Kara Sea based on the results of numerical modeling. A wave model WAVEWATCH III is used to reconstruct wind wave fields for the period from 1979 to 2017. The maximum significant wave height (SWH) for the whole period amounts to 9.9 m. The average long-term SWH for the ice-free period does not exceed 1.3 m. A significant linear trend shows an increase in the storm wave frequency for the period from 1979 to 2017. It is shown that trends in the storm activity of the Kara Sea are primarily regulated by the ice. Analysis of the extreme storm events showed that the Pareto distribution is in the best agreement with the data. However, the extreme events with an SWH more than 6‒7 m deviate from the Pareto distribution. Text Arctic Climate change Kara Sea Sea ice MDPI Open Access Publishing Arctic Kara Sea Water 13 5 648
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic the Kara Sea
wave climate
storm activity
wind waves
wave modeling
WAVEWATCH III
probabilistic analysis
extreme waves
spellingShingle the Kara Sea
wave climate
storm activity
wind waves
wave modeling
WAVEWATCH III
probabilistic analysis
extreme waves
Stanislav Myslenkov
Vladimir Platonov
Alexander Kislov
Ksenia Silvestrova
Igor Medvedev
Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
topic_facet the Kara Sea
wave climate
storm activity
wind waves
wave modeling
WAVEWATCH III
probabilistic analysis
extreme waves
description The recurrence of extreme wind waves in the Kara Sea strongly influences the Arctic climate change. The period 2000–2010 is characterized by significant climate warming, a reduction of the sea ice in the Arctic. The main motivation of this research to assess the impact of climate change on storm activity over the past 39 years in the Kara Sea. The paper presents the analysis of wave climate and storm activity in the Kara Sea based on the results of numerical modeling. A wave model WAVEWATCH III is used to reconstruct wind wave fields for the period from 1979 to 2017. The maximum significant wave height (SWH) for the whole period amounts to 9.9 m. The average long-term SWH for the ice-free period does not exceed 1.3 m. A significant linear trend shows an increase in the storm wave frequency for the period from 1979 to 2017. It is shown that trends in the storm activity of the Kara Sea are primarily regulated by the ice. Analysis of the extreme storm events showed that the Pareto distribution is in the best agreement with the data. However, the extreme events with an SWH more than 6‒7 m deviate from the Pareto distribution.
format Text
author Stanislav Myslenkov
Vladimir Platonov
Alexander Kislov
Ksenia Silvestrova
Igor Medvedev
author_facet Stanislav Myslenkov
Vladimir Platonov
Alexander Kislov
Ksenia Silvestrova
Igor Medvedev
author_sort Stanislav Myslenkov
title Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
title_short Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
title_full Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
title_fullStr Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
title_full_unstemmed Thirty-Nine-Year Wave Hindcast, Storm Activity, and Probability Analysis of Storm Waves in the Kara Sea, Russia
title_sort thirty-nine-year wave hindcast, storm activity, and probability analysis of storm waves in the kara sea, russia
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/w13050648
op_coverage agris
geographic Arctic
Kara Sea
geographic_facet Arctic
Kara Sea
genre Arctic
Climate change
Kara Sea
Sea ice
genre_facet Arctic
Climate change
Kara Sea
Sea ice
op_source Water; Volume 13; Issue 5; Pages: 648
op_relation Oceans and Coastal Zones
https://dx.doi.org/10.3390/w13050648
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/w13050648
container_title Water
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container_issue 5
container_start_page 648
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