Ice-Shelf Melting Around Antarctica
Major Meltdown The ice shelves and floating ice tongues that surround Antarctica cover more than 1.5 million square kilometers—approximately the size of the entire Greenland Ice Sheet. Conventional wisdom has held that ice shelves around Antarctica lose mass mostly by iceberg calving, but recently i...
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Online Access: | http://dx.doi.org/10.1126/science.1235798 https://www.science.org/doi/pdf/10.1126/science.1235798 |
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craaas:10.1126/science.1235798 2024-06-23T07:47:16+00:00 Ice-Shelf Melting Around Antarctica Rignot, E. Jacobs, S. Mouginot, J. Scheuchl, B. 2013 http://dx.doi.org/10.1126/science.1235798 https://www.science.org/doi/pdf/10.1126/science.1235798 en eng American Association for the Advancement of Science (AAAS) Science volume 341, issue 6143, page 266-270 ISSN 0036-8075 1095-9203 journal-article 2013 craaas https://doi.org/10.1126/science.1235798 2024-06-13T04:01:03Z Major Meltdown The ice shelves and floating ice tongues that surround Antarctica cover more than 1.5 million square kilometers—approximately the size of the entire Greenland Ice Sheet. Conventional wisdom has held that ice shelves around Antarctica lose mass mostly by iceberg calving, but recently it has become increasingly clear that melting by a warming ocean may also be important. Rignot et al. (p. 266 , published 13 June) present detailed glaciological estimates of ice-shelf melting around the entire continent of Antarctica, which show that basal melting accounts for as much mass loss as does calving. Article in Journal/Newspaper Antarc* Antarctica Greenland Ice Sheet Ice Shelf Ice Shelves AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 341 6143 266 270 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
Major Meltdown The ice shelves and floating ice tongues that surround Antarctica cover more than 1.5 million square kilometers—approximately the size of the entire Greenland Ice Sheet. Conventional wisdom has held that ice shelves around Antarctica lose mass mostly by iceberg calving, but recently it has become increasingly clear that melting by a warming ocean may also be important. Rignot et al. (p. 266 , published 13 June) present detailed glaciological estimates of ice-shelf melting around the entire continent of Antarctica, which show that basal melting accounts for as much mass loss as does calving. |
format |
Article in Journal/Newspaper |
author |
Rignot, E. Jacobs, S. Mouginot, J. Scheuchl, B. |
spellingShingle |
Rignot, E. Jacobs, S. Mouginot, J. Scheuchl, B. Ice-Shelf Melting Around Antarctica |
author_facet |
Rignot, E. Jacobs, S. Mouginot, J. Scheuchl, B. |
author_sort |
Rignot, E. |
title |
Ice-Shelf Melting Around Antarctica |
title_short |
Ice-Shelf Melting Around Antarctica |
title_full |
Ice-Shelf Melting Around Antarctica |
title_fullStr |
Ice-Shelf Melting Around Antarctica |
title_full_unstemmed |
Ice-Shelf Melting Around Antarctica |
title_sort |
ice-shelf melting around antarctica |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2013 |
url |
http://dx.doi.org/10.1126/science.1235798 https://www.science.org/doi/pdf/10.1126/science.1235798 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland Ice Sheet Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctica Greenland Ice Sheet Ice Shelf Ice Shelves |
op_source |
Science volume 341, issue 6143, page 266-270 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.1235798 |
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Science |
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341 |
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6143 |
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266 |
op_container_end_page |
270 |
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1802651358844682240 |