The Arctic Ocean is a landlocked basin, at present covered by perennial sea ice. During the past few decades a significant thinning and shrinking of the sea ice has been observed, and modelling studies indicate that the Arctic Ocean ice cover could, by the end of this century, almost disappear from...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.2428 2023-05-15T14:35:56+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.2428 http://www.geus.dk/publications/bull/nr10/nr10_p61-64.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.2428 http://www.geus.dk/publications/bull/nr10/nr10_p61-64.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/bull/nr10/nr10_p61-64.pdf text ftciteseerx 2016-01-08T10:16:53Z The Arctic Ocean is a landlocked basin, at present covered by perennial sea ice. During the past few decades a significant thinning and shrinking of the sea ice has been observed, and modelling studies indicate that the Arctic Ocean ice cover could, by the end of this century, almost disappear from most parts of the Arctic Ocean during peak summer seasons. It remains uncertain, however, whether the environmental changes are an enhanced greenhouse-warming signal or a result of natural (long-term) variability, but palaeoceano-graphic studies can contribute to our understanding of the natural variability of environmental parameters, e.g. sea-ice cover and oceanographic changes on time-scales of centuries to millennia. As part of the multidisciplinary EU project Greenland Arctic Shelf Ice and Climate Experiment (GreenICE), sedi- Text Arctic Arctic Ocean Greenland Sea ice Unknown Arctic Arctic Ocean Greenland |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
description |
The Arctic Ocean is a landlocked basin, at present covered by perennial sea ice. During the past few decades a significant thinning and shrinking of the sea ice has been observed, and modelling studies indicate that the Arctic Ocean ice cover could, by the end of this century, almost disappear from most parts of the Arctic Ocean during peak summer seasons. It remains uncertain, however, whether the environmental changes are an enhanced greenhouse-warming signal or a result of natural (long-term) variability, but palaeoceano-graphic studies can contribute to our understanding of the natural variability of environmental parameters, e.g. sea-ice cover and oceanographic changes on time-scales of centuries to millennia. As part of the multidisciplinary EU project Greenland Arctic Shelf Ice and Climate Experiment (GreenICE), sedi- |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.2428 http://www.geus.dk/publications/bull/nr10/nr10_p61-64.pdf |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Arctic Arctic Ocean Greenland Sea ice |
genre_facet |
Arctic Arctic Ocean Greenland Sea ice |
op_source |
http://www.geus.dk/publications/bull/nr10/nr10_p61-64.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.2428 http://www.geus.dk/publications/bull/nr10/nr10_p61-64.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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1766308670020255744 |