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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Main Authors: Song, Zhaoyang, Latif, Mojib, Park, Wonsun
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.877918
https://doi.pangaea.de/10.1594/PANGAEA.877918
id ftdatacite:10.1594/pangaea.877918
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic File content
File name
File format
File size
Uniform resource locator/link to model result file
spellingShingle 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 ...
topic_facet 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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