the Chukchi Sea into the Arctic Ocean in
Four days of current record were obtained about 190 km NNE of Bering Strait during Mcarch 1968. The mean current was the same for the location as in summer, suggesting that the generally north flow from the Bering Sea to the Arctic Ocean occurs also in winter. Variations in speed and direction of th...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.500.6767 2023-05-15T14:53:28+02:00 the Chukchi Sea into the Arctic Ocean in L. K. Coachman The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.6767 http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.6767 http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf dominantly north through Bering Strait and text ftciteseerx 2016-01-08T09:07:09Z Four days of current record were obtained about 190 km NNE of Bering Strait during Mcarch 1968. The mean current was the same for the location as in summer, suggesting that the generally north flow from the Bering Sea to the Arctic Ocean occurs also in winter. Variations in speed and direction of the flow were identified and analyzed. The major periodic variation was due to the diurnal tidal wave, and thus the tidal wave rather than inertial currents must be the primary cause of periodic variations. The course of the tidal wave and some features of its behavior are inferred. Other variations of importjnce include a variation with a period somewhat greater than 2 days, probably caused by atmospheric Dhenomena. and fluctuations due to relatively large-scale turbulence (periods between 5 ind 60 mii). Text Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Chukchi Sea Unknown Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Sea |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
topic |
dominantly north through Bering Strait and |
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dominantly north through Bering Strait and L. K. Coachman the Chukchi Sea into the Arctic Ocean in |
topic_facet |
dominantly north through Bering Strait and |
description |
Four days of current record were obtained about 190 km NNE of Bering Strait during Mcarch 1968. The mean current was the same for the location as in summer, suggesting that the generally north flow from the Bering Sea to the Arctic Ocean occurs also in winter. Variations in speed and direction of the flow were identified and analyzed. The major periodic variation was due to the diurnal tidal wave, and thus the tidal wave rather than inertial currents must be the primary cause of periodic variations. The course of the tidal wave and some features of its behavior are inferred. Other variations of importjnce include a variation with a period somewhat greater than 2 days, probably caused by atmospheric Dhenomena. and fluctuations due to relatively large-scale turbulence (periods between 5 ind 60 mii). |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
L. K. Coachman |
author_facet |
L. K. Coachman |
author_sort |
L. K. Coachman |
title |
the Chukchi Sea into the Arctic Ocean in |
title_short |
the Chukchi Sea into the Arctic Ocean in |
title_full |
the Chukchi Sea into the Arctic Ocean in |
title_fullStr |
the Chukchi Sea into the Arctic Ocean in |
title_full_unstemmed |
the Chukchi Sea into the Arctic Ocean in |
title_sort |
chukchi sea into the arctic ocean in |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.6767 http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf |
geographic |
Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Sea |
geographic_facet |
Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Sea |
genre |
Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Chukchi Sea |
genre_facet |
Arctic Arctic Ocean Bering Sea Bering Strait Chukchi Chukchi Sea |
op_source |
http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.500.6767 http://www.aslo.org/lo/toc/vol_15/issue_4/0625.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766325034952949760 |