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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Published in:Geophysical Research Letters
Main Authors: Fyke, J.G. (author), Vizcaino, M. (author), Lipscomb, W.H. (author)
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2014
Subjects:
Online Access:https://doi.org/10.1002/2014GL060735
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spelling 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
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