be “coupled.” Furthermore, under the current atmo-spheric state, there are strong southerly winds over the Norwegian Sea, and hence the wind-driven inflow of warm Atlantic water into the Arctic is relatively strong, penetrating far into the central Arctic Basin (11). Any pollutants entering the ocea...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6136 http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1027.6136 2023-05-15T14:29:06+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6136 http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6136 http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf text ftciteseerx 2016-10-30T00:04:57Z be “coupled.” Furthermore, under the current atmo-spheric state, there are strong southerly winds over the Norwegian Sea, and hence the wind-driven inflow of warm Atlantic water into the Arctic is relatively strong, penetrating far into the central Arctic Basin (11). Any pollutants entering the ocean from Western Europe could thus penetrate far into the Arctic and might even reach the Canadian Basin. In con-trast, during the 1950s to 1980s, when the three indices were mainly negative, the At-lantic inflow would not have penetrated very far into the Arctic Basin. Text Arctic Basin Arctic Norwegian Sea Unknown Arctic Norwegian Sea |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
be “coupled.” Furthermore, under the current atmo-spheric state, there are strong southerly winds over the Norwegian Sea, and hence the wind-driven inflow of warm Atlantic water into the Arctic is relatively strong, penetrating far into the central Arctic Basin (11). Any pollutants entering the ocean from Western Europe could thus penetrate far into the Arctic and might even reach the Canadian Basin. In con-trast, during the 1950s to 1980s, when the three indices were mainly negative, the At-lantic inflow would not have penetrated very far into the Arctic Basin. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6136 http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf |
geographic |
Arctic Norwegian Sea |
geographic_facet |
Arctic Norwegian Sea |
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Arctic Basin Arctic Norwegian Sea |
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Arctic Basin Arctic Norwegian Sea |
op_source |
http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6136 http://science.sciencemag.org/content/sci/293/5533/1270.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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