Summertime gap winds of the Soya Strait induced by the developed Okhotsk high

Abstract This study has investigated gap winds to the west of the Soya Strait during the summer months. Low‐level cool air associated with the developed Okhotsk high is dammed on the east sides of Sakhalin and Hokkaido, and enhances sea level pressure (SLP) gradient along the Soya Strait on a region...

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Published in:Atmospheric Science Letters
Main Authors: Shimada, Teruhisa, Kawamura, Hiroshi
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
Subjects:
Online Access:http://dx.doi.org/10.1002/asl.345
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spelling crwiley:10.1002/asl.345 2024-06-02T08:12:41+00:00 Summertime gap winds of the Soya Strait induced by the developed Okhotsk high Shimada, Teruhisa Kawamura, Hiroshi 2011 http://dx.doi.org/10.1002/asl.345 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.345 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.345 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Atmospheric Science Letters volume 12, issue 3, page 316-320 ISSN 1530-261X 1530-261X journal-article 2011 crwiley https://doi.org/10.1002/asl.345 2024-05-03T11:32:10Z Abstract This study has investigated gap winds to the west of the Soya Strait during the summer months. Low‐level cool air associated with the developed Okhotsk high is dammed on the east sides of Sakhalin and Hokkaido, and enhances sea level pressure (SLP) gradient along the Soya Strait on a regional scale. The Soya Strait works as a conduit for the cool air from the Okhotsk Sea to the Japan Sea, and the outflowing air accelerates because of the along‐strait SLP gradient. The intensity and duration time of the easterly gap winds depend on the activity of the Okhotsk high. Copyright © 2011 Royal Meteorological Society Article in Journal/Newspaper okhotsk sea Sakhalin Wiley Online Library Okhotsk Atmospheric Science Letters 12 3 316 320
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This study has investigated gap winds to the west of the Soya Strait during the summer months. Low‐level cool air associated with the developed Okhotsk high is dammed on the east sides of Sakhalin and Hokkaido, and enhances sea level pressure (SLP) gradient along the Soya Strait on a regional scale. The Soya Strait works as a conduit for the cool air from the Okhotsk Sea to the Japan Sea, and the outflowing air accelerates because of the along‐strait SLP gradient. The intensity and duration time of the easterly gap winds depend on the activity of the Okhotsk high. Copyright © 2011 Royal Meteorological Society
format Article in Journal/Newspaper
author Shimada, Teruhisa
Kawamura, Hiroshi
spellingShingle Shimada, Teruhisa
Kawamura, Hiroshi
Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
author_facet Shimada, Teruhisa
Kawamura, Hiroshi
author_sort Shimada, Teruhisa
title Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
title_short Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
title_full Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
title_fullStr Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
title_full_unstemmed Summertime gap winds of the Soya Strait induced by the developed Okhotsk high
title_sort summertime gap winds of the soya strait induced by the developed okhotsk high
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/asl.345
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.345
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.345
geographic Okhotsk
geographic_facet Okhotsk
genre okhotsk sea
Sakhalin
genre_facet okhotsk sea
Sakhalin
op_source Atmospheric Science Letters
volume 12, issue 3, page 316-320
ISSN 1530-261X 1530-261X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/asl.345
container_title Atmospheric Science Letters
container_volume 12
container_issue 3
container_start_page 316
op_container_end_page 320
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