Hokkaido Central Fisheries Experimental Station
The Soya Warm Current is the only supplier of saline subtropical water to the Okhotsk Sea. The Soya Warm Water obtains high density values comparative to NPIW (North Pacific Intermediate Water) by winter cooling, due to its high salinity value, and may influence the intermediate water in the Okhotsk...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.359.8974 2023-05-15T17:52:34+02:00 Hokkaido Central Fisheries Experimental Station Andrew D. Samatov The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.359.8974 http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.359.8974 http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf text ftciteseerx 2016-01-08T00:45:04Z The Soya Warm Current is the only supplier of saline subtropical water to the Okhotsk Sea. The Soya Warm Water obtains high density values comparative to NPIW (North Pacific Intermediate Water) by winter cooling, due to its high salinity value, and may influence the intermediate water in the Okhotsk Sea, which is considered as a source water of NPIW. However, as the northern half of the La Perouse Strait (the Soya Strait) belongs to Russia and the southern half to Japan, no observations across the strait have been made except in the period before the World War II. The vertical resolution and spatial coverage of these old observations are very limited, and the accuracy of the measurement is also very limited due to instruments used in those days. The Joint Text okhotsk sea Unknown Okhotsk Pacific |
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ftciteseerx |
language |
English |
description |
The Soya Warm Current is the only supplier of saline subtropical water to the Okhotsk Sea. The Soya Warm Water obtains high density values comparative to NPIW (North Pacific Intermediate Water) by winter cooling, due to its high salinity value, and may influence the intermediate water in the Okhotsk Sea, which is considered as a source water of NPIW. However, as the northern half of the La Perouse Strait (the Soya Strait) belongs to Russia and the southern half to Japan, no observations across the strait have been made except in the period before the World War II. The vertical resolution and spatial coverage of these old observations are very limited, and the accuracy of the measurement is also very limited due to instruments used in those days. The Joint |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Andrew D. Samatov |
spellingShingle |
Andrew D. Samatov Hokkaido Central Fisheries Experimental Station |
author_facet |
Andrew D. Samatov |
author_sort |
Andrew D. Samatov |
title |
Hokkaido Central Fisheries Experimental Station |
title_short |
Hokkaido Central Fisheries Experimental Station |
title_full |
Hokkaido Central Fisheries Experimental Station |
title_fullStr |
Hokkaido Central Fisheries Experimental Station |
title_full_unstemmed |
Hokkaido Central Fisheries Experimental Station |
title_sort |
hokkaido central fisheries experimental station |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.359.8974 http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf |
geographic |
Okhotsk Pacific |
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Okhotsk Pacific |
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okhotsk sea |
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okhotsk sea |
op_source |
http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.359.8974 http://www.pices.int/publications/scientific_reports/Report12/nakata_revf.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766160131322544128 |