Ice Sheets
Ice sheets are dome‐shaped continental glaciers up to several kilometers thick and covering at least 50 000 km 2 . The two current ice sheets are located in Greenland and Antarctica. Two additional ice masses existed 20 000 years ago, the Laurentide and Fennoscandian ice sheets, which left their imp...
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crwiley:10.1002/9781118786352.wbieg0819 2024-10-06T13:44:19+00:00 Ice Sheets André, Marie‐Françoise 2017 http://dx.doi.org/10.1002/9781118786352.wbieg0819 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F9781118786352.wbieg0819 https://onlinelibrary.wiley.com/doi/pdf/10.1002/9781118786352.wbieg0819 en eng Wiley http://doi.wiley.com/10.1002/tdm_license_1.1 http://doi.wiley.com/10.1002/tdm_license_1.1 International Encyclopedia of Geography page 1-5 ISBN 9780470659632 9781118786352 other 2017 crwiley https://doi.org/10.1002/9781118786352.wbieg0819 2024-09-11T04:14:10Z Ice sheets are dome‐shaped continental glaciers up to several kilometers thick and covering at least 50 000 km 2 . The two current ice sheets are located in Greenland and Antarctica. Two additional ice masses existed 20 000 years ago, the Laurentide and Fennoscandian ice sheets, which left their imprint on Nordic landscapes. Ice sheets contain a unique record of the Earth 's climate history provided by air bubbles trapped in the ice during the last 800 000 years. According to emission scenarios and mass balance estimations, models suggest that the current accelerated ice loss from Greenland and West Antarctica will continue and probably cause a sea level rise of 12 cm and 5 cm respectively by 2100. Geomorphological evidence, the marine sediment record, and glaciological modeling indicate a long‐term stability of the East Antarctic Ice Sheet. Other/Unknown Material Antarc* Antarctic Antarctica Fennoscandian Greenland Ice Sheet West Antarctica Wiley Online Library Antarctic East Antarctic Ice Sheet Greenland West Antarctica 1 5 |
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Wiley Online Library |
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English |
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Ice sheets are dome‐shaped continental glaciers up to several kilometers thick and covering at least 50 000 km 2 . The two current ice sheets are located in Greenland and Antarctica. Two additional ice masses existed 20 000 years ago, the Laurentide and Fennoscandian ice sheets, which left their imprint on Nordic landscapes. Ice sheets contain a unique record of the Earth 's climate history provided by air bubbles trapped in the ice during the last 800 000 years. According to emission scenarios and mass balance estimations, models suggest that the current accelerated ice loss from Greenland and West Antarctica will continue and probably cause a sea level rise of 12 cm and 5 cm respectively by 2100. Geomorphological evidence, the marine sediment record, and glaciological modeling indicate a long‐term stability of the East Antarctic Ice Sheet. |
format |
Other/Unknown Material |
author |
André, Marie‐Françoise |
spellingShingle |
André, Marie‐Françoise Ice Sheets |
author_facet |
André, Marie‐Françoise |
author_sort |
André, Marie‐Françoise |
title |
Ice Sheets |
title_short |
Ice Sheets |
title_full |
Ice Sheets |
title_fullStr |
Ice Sheets |
title_full_unstemmed |
Ice Sheets |
title_sort |
ice sheets |
publisher |
Wiley |
publishDate |
2017 |
url |
http://dx.doi.org/10.1002/9781118786352.wbieg0819 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F9781118786352.wbieg0819 https://onlinelibrary.wiley.com/doi/pdf/10.1002/9781118786352.wbieg0819 |
geographic |
Antarctic East Antarctic Ice Sheet Greenland West Antarctica |
geographic_facet |
Antarctic East Antarctic Ice Sheet Greenland West Antarctica |
genre |
Antarc* Antarctic Antarctica Fennoscandian Greenland Ice Sheet West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Fennoscandian Greenland Ice Sheet West Antarctica |
op_source |
International Encyclopedia of Geography page 1-5 ISBN 9780470659632 9781118786352 |
op_rights |
http://doi.wiley.com/10.1002/tdm_license_1.1 http://doi.wiley.com/10.1002/tdm_license_1.1 |
op_doi |
https://doi.org/10.1002/9781118786352.wbieg0819 |
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