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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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 |
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Open Polar |
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Wiley Online Library |
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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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1800759213498040320 |