Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ...
Proxy data suggest that the Plio-Pleistocene transition from ~3.2 - 3.0 to 2.5 Ma featured the onset of Northern Hemisphere glaciation and enhanced climate variability on obliquity timescale. Here, we investigate the influence of the expanding Greenland ice sheet (GrIS) on the mean climate and obliq...
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ftdatacite:10.1594/pangaea.877918 2024-09-15T18:08:48+00:00 Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... Song, Zhaoyang Latif, Mojib Park, Wonsun 2017 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.877918 https://doi.pangaea.de/10.1594/PANGAEA.877918 en eng PANGAEA https://dx.doi.org/10.1002/2017gl074835 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 File content File name File format File size Uniform resource locator/link to model result file dataset Supplementary Dataset Dataset 2017 ftdatacite https://doi.org/10.1594/pangaea.87791810.1002/2017gl074835 2024-08-01T11:01:20Z Proxy data suggest that the Plio-Pleistocene transition from ~3.2 - 3.0 to 2.5 Ma featured the onset of Northern Hemisphere glaciation and enhanced climate variability on obliquity timescale. Here, we investigate the influence of the expanding Greenland ice sheet (GrIS) on the mean climate and obliquity-related variability. Special attention is given to the Atlantic Meridional Overturning Circulation (AMOC). A series of climate model simulations suggest that the expanding GrIS weakens the AMOC by ~1 Sv, which is mainly due to reduced heat loss of the Greenland-Iceland-Norwegian Sea. Moreover, the expanded GrIS amplifies the Hadley circulation response to obliquity forcing. This drives enhanced obliquity-forced variations in freshwater export from the tropical Atlantic and in turn variations of the AMOC that increase by about a factor. The stronger AMOC response to obliquity forcing in turn drives a stronger global-mean near-surface temperature response. We conclude that the AMOC response to obliquity forcing ... : Supplement to: Song, Zhaoyang; Latif, Mojib; Park, Wonsun (2017): Expanding Greenland Ice Sheet Enhances Sensitivity of Plio-Pleistocene Climate to Obliquity Forcing in the Kiel Climate Model. Geophysical Research Letters ... Dataset Greenland Ice Sheet Iceland Norwegian Sea DataCite |
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English |
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File content File name File format File size Uniform resource locator/link to model result file |
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File content File name File format File size Uniform resource locator/link to model result file Song, Zhaoyang Latif, Mojib Park, Wonsun Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
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File content File name File format File size Uniform resource locator/link to model result file |
description |
Proxy data suggest that the Plio-Pleistocene transition from ~3.2 - 3.0 to 2.5 Ma featured the onset of Northern Hemisphere glaciation and enhanced climate variability on obliquity timescale. Here, we investigate the influence of the expanding Greenland ice sheet (GrIS) on the mean climate and obliquity-related variability. Special attention is given to the Atlantic Meridional Overturning Circulation (AMOC). A series of climate model simulations suggest that the expanding GrIS weakens the AMOC by ~1 Sv, which is mainly due to reduced heat loss of the Greenland-Iceland-Norwegian Sea. Moreover, the expanded GrIS amplifies the Hadley circulation response to obliquity forcing. This drives enhanced obliquity-forced variations in freshwater export from the tropical Atlantic and in turn variations of the AMOC that increase by about a factor. The stronger AMOC response to obliquity forcing in turn drives a stronger global-mean near-surface temperature response. We conclude that the AMOC response to obliquity forcing ... : Supplement to: Song, Zhaoyang; Latif, Mojib; Park, Wonsun (2017): Expanding Greenland Ice Sheet Enhances Sensitivity of Plio-Pleistocene Climate to Obliquity Forcing in the Kiel Climate Model. Geophysical Research Letters ... |
format |
Dataset |
author |
Song, Zhaoyang Latif, Mojib Park, Wonsun |
author_facet |
Song, Zhaoyang Latif, Mojib Park, Wonsun |
author_sort |
Song, Zhaoyang |
title |
Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
title_short |
Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
title_full |
Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
title_fullStr |
Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
title_full_unstemmed |
Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model ... |
title_sort |
simulated mean climate response to expanded greenland ice sheet in the kiel climate model ... |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.877918 https://doi.pangaea.de/10.1594/PANGAEA.877918 |
genre |
Greenland Ice Sheet Iceland Norwegian Sea |
genre_facet |
Greenland Ice Sheet Iceland Norwegian Sea |
op_relation |
https://dx.doi.org/10.1002/2017gl074835 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.87791810.1002/2017gl074835 |
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1810446172023685120 |