sin er wa re
doi:10.1098/rsta.2006.1794 Published online 26 May 2006consistent with increased melting of continental ice. Newly forming bottom water has become colder and less salty downstream from that region, but generally warmer in the Weddell Sea. Many ice shelves have retreated or thinned, but others have g...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.466.2106 2023-05-15T13:49:19+02:00 sin er wa re The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.466.2106 http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.466.2106 http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.pdf ocean freshening and warming text ftciteseerx 2016-01-08T06:55:53Z doi:10.1098/rsta.2006.1794 Published online 26 May 2006consistent with increased melting of continental ice. Newly forming bottom water has become colder and less salty downstream from that region, but generally warmer in the Weddell Sea. Many ice shelves have retreated or thinned, but others have grown and no trend is apparent in the large iceberg calving rate. Warming and isotherm shoaling within the polar gyres may result in part from changes in the Southern Annular Mode, which could facilitate deep-water access to the continental shelves. Sea-level rise over the past half century has a strong eustatic component and has recently accelerated. Observations over longer periods and with better spatial coverage are needed to better understand the processes causing these changes and their links to the Antarctic ice sheet. Text Antarc* Antarctic Ice Sheet Ice Shelves Iceberg* Weddell Sea Unknown Antarctic The Antarctic Weddell Sea Weddell |
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ocean freshening and warming |
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ocean freshening and warming sin er wa re |
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ocean freshening and warming |
description |
doi:10.1098/rsta.2006.1794 Published online 26 May 2006consistent with increased melting of continental ice. Newly forming bottom water has become colder and less salty downstream from that region, but generally warmer in the Weddell Sea. Many ice shelves have retreated or thinned, but others have grown and no trend is apparent in the large iceberg calving rate. Warming and isotherm shoaling within the polar gyres may result in part from changes in the Southern Annular Mode, which could facilitate deep-water access to the continental shelves. Sea-level rise over the past half century has a strong eustatic component and has recently accelerated. Observations over longer periods and with better spatial coverage are needed to better understand the processes causing these changes and their links to the Antarctic ice sheet. |
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The Pennsylvania State University CiteSeerX Archives |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.466.2106 http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.pdf |
geographic |
Antarctic The Antarctic Weddell Sea Weddell |
geographic_facet |
Antarctic The Antarctic Weddell Sea Weddell |
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Antarc* Antarctic Ice Sheet Ice Shelves Iceberg* Weddell Sea |
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Antarc* Antarctic Ice Sheet Ice Shelves Iceberg* Weddell Sea |
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http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.466.2106 http://www.ldeo.columbia.edu/~irina/lamont/paper1_stan/Jacobs2006_SouthOcChange.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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