Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures
[1] The spatial and temporal evolution of winter sea ice anomalies in the Labrador Sea and associated sea surface temperature (SST) variations in the North Atlantic are documented for three periods of above-normal ice cover: 1972–1974, 1983–1985, and 1990–1992. These events are notable for their win...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.384.4262 2023-05-15T15:35:05+02:00 Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures Clara Deser Marika Holl Gilles Reverdin Michael Timlin The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.4262 http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.4262 http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.pdf text ftciteseerx 2016-09-18T00:29:58Z [1] The spatial and temporal evolution of winter sea ice anomalies in the Labrador Sea and associated sea surface temperature (SST) variations in the North Atlantic are documented for three periods of above-normal ice cover: 1972–1974, 1983–1985, and 1990–1992. These events are notable for their winter-to-winter persistence, despite the fact that the ice margin retreats to northern Baffin Bay each summer, and for their spatial evolution, progressing from the northern Labrador Sea to the southern tip of Newfoundland over a 3 year period. Abovenormal sea ice is consistently accompanied by below-normal SSTs in the subpolar Atlantic: the latter persist 1–3 years after the decay of the ice anomalies and in some cases exhibit a tendency for eastward movement across the gyre. Spring–summer freshwater anomalies at 100 m depth in the West Greenland Current are found to precede by 8 months the initial occurrence of above-normal ice cover in the northern Labrador Sea. The role of atmospheric forcing in the joint evolution of anomalous sea ice and SST is assessed by means of an iceocean mixed layer model forced with observed air temperature and wind fields. The model results indicate that thermodynamic atmospheric forcing accounts for much of the winter-towinter persistence and spatial evolution of the ice and concurrent SST anomaly patterns. Text Baffin Bay Baffin Bay Baffin Greenland Labrador Sea Newfoundland North Atlantic Sea ice Unknown Newfoundland Baffin Bay Greenland |
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English |
description |
[1] The spatial and temporal evolution of winter sea ice anomalies in the Labrador Sea and associated sea surface temperature (SST) variations in the North Atlantic are documented for three periods of above-normal ice cover: 1972–1974, 1983–1985, and 1990–1992. These events are notable for their winter-to-winter persistence, despite the fact that the ice margin retreats to northern Baffin Bay each summer, and for their spatial evolution, progressing from the northern Labrador Sea to the southern tip of Newfoundland over a 3 year period. Abovenormal sea ice is consistently accompanied by below-normal SSTs in the subpolar Atlantic: the latter persist 1–3 years after the decay of the ice anomalies and in some cases exhibit a tendency for eastward movement across the gyre. Spring–summer freshwater anomalies at 100 m depth in the West Greenland Current are found to precede by 8 months the initial occurrence of above-normal ice cover in the northern Labrador Sea. The role of atmospheric forcing in the joint evolution of anomalous sea ice and SST is assessed by means of an iceocean mixed layer model forced with observed air temperature and wind fields. The model results indicate that thermodynamic atmospheric forcing accounts for much of the winter-towinter persistence and spatial evolution of the ice and concurrent SST anomaly patterns. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Clara Deser Marika Holl Gilles Reverdin Michael Timlin |
spellingShingle |
Clara Deser Marika Holl Gilles Reverdin Michael Timlin Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
author_facet |
Clara Deser Marika Holl Gilles Reverdin Michael Timlin |
author_sort |
Clara Deser |
title |
Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
title_short |
Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
title_full |
Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
title_fullStr |
Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
title_full_unstemmed |
Decadal variations in Labrador Sea ice cover and North Atlantic sea surface temperatures |
title_sort |
decadal variations in labrador sea ice cover and north atlantic sea surface temperatures |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.4262 http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.pdf |
geographic |
Newfoundland Baffin Bay Greenland |
geographic_facet |
Newfoundland Baffin Bay Greenland |
genre |
Baffin Bay Baffin Bay Baffin Greenland Labrador Sea Newfoundland North Atlantic Sea ice |
genre_facet |
Baffin Bay Baffin Bay Baffin Greenland Labrador Sea Newfoundland North Atlantic Sea ice |
op_source |
http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.4262 http://www.cgd.ucar.edu/cas/cdeser/Docs/deser.labradorseaice.jclim02.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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1766365385675767808 |