The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance
Surface mass balance (SMB) trends influence observed Greenland Ice Sheet (GrIS) mass loss, but the component of these trends related to anthropogenic forcing is unclear. Here we study the simulated spatial pattern of emergence of an anthropogenically derived GrIS SMB signal between 1850 and 2100 usi...
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American Geophysical Union
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Online Access: | https://doi.org/10.1002/2014GL060735 http://resolver.tudelft.nl/uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 |
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fttudelft:oai:tudelft.nl:uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 2023-07-30T04:03:46+02:00 The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance Fyke, J.G. (author) Vizcaino, M. (author) Lipscomb, W.H. (author) 2014-08-18 https://doi.org/10.1002/2014GL060735 http://resolver.tudelft.nl/uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 en eng American Geophysical Union Geophysical Research Letters, 41 (16), 2014--0094-8276 https://doi.org/10.1002/2014GL060735 http://resolver.tudelft.nl/uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 © 2014 American Geophysical Union Greenland surface mass balance anthropogenic signal climate change cryosphere journal article Text 2014 fttudelft https://doi.org/10.1002/2014GL060735 2023-07-08T20:18:11Z Surface mass balance (SMB) trends influence observed Greenland Ice Sheet (GrIS) mass loss, but the component of these trends related to anthropogenic forcing is unclear. Here we study the simulated spatial pattern of emergence of an anthropogenically derived GrIS SMB signal between 1850 and 2100 using the Community Earth System Model. We find emergence timing heterogeneity, with a bimodal structure reflecting interior snowfall increases against a background of low SMB variability, and peripheral surface melting increases against a backdrop of high SMB variability. We also find a nonemerging intermediate region. We conclude that (1) a bimodal pattern of GrIS SMB change will unambiguously reflect the impact of anthropogenic forcing; (2) present-day peripheral and interior SMB trends likely have an underlying anthropogenically forced component; (3) local emergence occurs well before emergence of a spatially integrated signal; and (4) the GrIS summit region may be an ideal location for monitoring regional/global climate change. Geoscience & Remote Sensing Civil Engineering and Geosciences Article in Journal/Newspaper Greenland Ice Sheet Delft University of Technology: Institutional Repository Greenland Geophysical Research Letters 41 16 6002 6008 |
institution |
Open Polar |
collection |
Delft University of Technology: Institutional Repository |
op_collection_id |
fttudelft |
language |
English |
topic |
Greenland surface mass balance anthropogenic signal climate change cryosphere |
spellingShingle |
Greenland surface mass balance anthropogenic signal climate change cryosphere Fyke, J.G. (author) Vizcaino, M. (author) Lipscomb, W.H. (author) The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
topic_facet |
Greenland surface mass balance anthropogenic signal climate change cryosphere |
description |
Surface mass balance (SMB) trends influence observed Greenland Ice Sheet (GrIS) mass loss, but the component of these trends related to anthropogenic forcing is unclear. Here we study the simulated spatial pattern of emergence of an anthropogenically derived GrIS SMB signal between 1850 and 2100 using the Community Earth System Model. We find emergence timing heterogeneity, with a bimodal structure reflecting interior snowfall increases against a background of low SMB variability, and peripheral surface melting increases against a backdrop of high SMB variability. We also find a nonemerging intermediate region. We conclude that (1) a bimodal pattern of GrIS SMB change will unambiguously reflect the impact of anthropogenic forcing; (2) present-day peripheral and interior SMB trends likely have an underlying anthropogenically forced component; (3) local emergence occurs well before emergence of a spatially integrated signal; and (4) the GrIS summit region may be an ideal location for monitoring regional/global climate change. Geoscience & Remote Sensing Civil Engineering and Geosciences |
format |
Article in Journal/Newspaper |
author |
Fyke, J.G. (author) Vizcaino, M. (author) Lipscomb, W.H. (author) |
author_facet |
Fyke, J.G. (author) Vizcaino, M. (author) Lipscomb, W.H. (author) |
author_sort |
Fyke, J.G. (author) |
title |
The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
title_short |
The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
title_full |
The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
title_fullStr |
The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
title_full_unstemmed |
The pattern of anthropogenic signal emergence in Greenland Ice Sheet surface mass balance |
title_sort |
pattern of anthropogenic signal emergence in greenland ice sheet surface mass balance |
publisher |
American Geophysical Union |
publishDate |
2014 |
url |
https://doi.org/10.1002/2014GL060735 http://resolver.tudelft.nl/uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_relation |
Geophysical Research Letters, 41 (16), 2014--0094-8276 https://doi.org/10.1002/2014GL060735 http://resolver.tudelft.nl/uuid:ae3e1d1a-fefc-4a05-96a7-978bc2c902f4 |
op_rights |
© 2014 American Geophysical Union |
op_doi |
https://doi.org/10.1002/2014GL060735 |
container_title |
Geophysical Research Letters |
container_volume |
41 |
container_issue |
16 |
container_start_page |
6002 |
op_container_end_page |
6008 |
_version_ |
1772814857144369152 |