Second, local and small-scale openings in the ice cover (polynyas) provide the necessary brine release for dense bottom waters. The polynyas open frequently near Franz Josef Land and Novaya Zemlya due to oV-shore winds. Tidal currents, however, may also play a role in opening the closed ice sheet. T...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.550.3270 http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.550.3270 2023-05-15T14:48:57+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.550.3270 http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.550.3270 http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf Key words Arctic Barents Sea water mass transformation text ftciteseerx 2016-01-08T11:31:30Z Second, local and small-scale openings in the ice cover (polynyas) provide the necessary brine release for dense bottom waters. The polynyas open frequently near Franz Josef Land and Novaya Zemlya due to oV-shore winds. Tidal currents, however, may also play a role in opening the closed ice sheet. Tracer studies reveal that most of the bottom water leaves the Barents Sea through the Svyataya Anna Trough towards the Arctic Ocean. Outflow rates of the deep water as well as the temporal and spatial evolution of stratification and ice cover are presented. Text Arctic Arctic Ocean Barents Sea Franz Josef Land Ice Sheet Novaya Zemlya Unknown Arctic Arctic Ocean Barents Sea Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Svyataya Anna Trough ENVELOPE(70.000,70.000,80.000,80.000) |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| topic |
Key words Arctic Barents Sea water mass transformation |
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Key words Arctic Barents Sea water mass transformation |
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Key words Arctic Barents Sea water mass transformation |
| description |
Second, local and small-scale openings in the ice cover (polynyas) provide the necessary brine release for dense bottom waters. The polynyas open frequently near Franz Josef Land and Novaya Zemlya due to oV-shore winds. Tidal currents, however, may also play a role in opening the closed ice sheet. Tracer studies reveal that most of the bottom water leaves the Barents Sea through the Svyataya Anna Trough towards the Arctic Ocean. Outflow rates of the deep water as well as the temporal and spatial evolution of stratification and ice cover are presented. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.550.3270 http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf |
| long_lat |
ENVELOPE(55.000,55.000,81.000,81.000) ENVELOPE(70.000,70.000,80.000,80.000) |
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Arctic Arctic Ocean Barents Sea Franz Josef Land Svyataya Anna Trough |
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Arctic Arctic Ocean Barents Sea Franz Josef Land Svyataya Anna Trough |
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Arctic Arctic Ocean Barents Sea Franz Josef Land Ice Sheet Novaya Zemlya |
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Arctic Arctic Ocean Barents Sea Franz Josef Land Ice Sheet Novaya Zemlya |
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http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.550.3270 http://icesjms.oxfordjournals.org/content/54/3/351.full.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766320029563879424 |