Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries
Most of the IPCC-AR4 Atmospheric Global Circulation Models (AGCM) predict an increase of the Antarctic Surface Mass Balance (SMB) during the 21st century that would mitigate global sea level rise. Present accumulation and predicted change are largest at the ice sheet margins because they are driven...
Main Authors: | , , , , |
---|---|
Format: | Conference Object |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | https://orbi.uliege.be/handle/2268/145011 https://orbi.uliege.be/bitstream/2268/145011/1/SCAR-2012.pdf |
id |
ftorbi:oai:orbi.ulg.ac.be:2268/145011 |
---|---|
record_format |
openpolar |
spelling |
ftorbi:oai:orbi.ulg.ac.be:2268/145011 2024-04-21T07:47:57+00:00 Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries Agosta, Cécile Favier, Vincent Krinner, Gerhard Gallée, Hubert Genthon, Christophe 2012-07 https://orbi.uliege.be/handle/2268/145011 https://orbi.uliege.be/bitstream/2268/145011/1/SCAR-2012.pdf en eng https://orbi.uliege.be/handle/2268/145011 info:hdl:2268/145011 https://orbi.uliege.be/bitstream/2268/145011/1/SCAR-2012.pdf open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess XXXII SCAR and Open Science Conference, Portland, Oregon, United States [US], du 13 au 19 juillet 2012 Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique conference paper not in proceedings http://purl.org/coar/resource_type/c_18cp info:eu-repo/semantics/conferencePaper 2012 ftorbi 2024-03-27T14:45:06Z Most of the IPCC-AR4 Atmospheric Global Circulation Models (AGCM) predict an increase of the Antarctic Surface Mass Balance (SMB) during the 21st century that would mitigate global sea level rise. Present accumulation and predicted change are largest at the ice sheet margins because they are driven by snowfall, which mostly comes from warm, moist air arising over the land slopes. The coastal belt is also where complex processes of sublimation, melt and refreezing occur. Thus, high-resolution modelling is necessary to adequately capture the effects of small-scale variations in topography on the atmospheric variables in this area, but limitations in computing resources prevent such resolution at the scale of Antarctica in full climate models. We present here a downscaling method leading to 15-km SMB resolution for century time-scales over Antarctica. We compute the effect of the fine topography on orographic precipitation and on boundary layer processes that lead to sublimation, melt and refreezing. We first display the SMB downscaled from ERA-Interim and show that the downscaling improves the agreement between modelled and observed SMB for the end of the 20th century. We then present hi-resolution features of the Antarctic SMB evolution during the 21st century downscaled from LMDZ4 for different scenarios. We show that a higher resolution induce at the same time more run-off but a significantly higher mitigation of sea level rise. Conference Object Antarc* Antarctic Antarctica Ice Sheet University of Liège: ORBi (Open Repository and Bibliography) |
institution |
Open Polar |
collection |
University of Liège: ORBi (Open Repository and Bibliography) |
op_collection_id |
ftorbi |
language |
English |
topic |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
spellingShingle |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique Agosta, Cécile Favier, Vincent Krinner, Gerhard Gallée, Hubert Genthon, Christophe Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
topic_facet |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
description |
Most of the IPCC-AR4 Atmospheric Global Circulation Models (AGCM) predict an increase of the Antarctic Surface Mass Balance (SMB) during the 21st century that would mitigate global sea level rise. Present accumulation and predicted change are largest at the ice sheet margins because they are driven by snowfall, which mostly comes from warm, moist air arising over the land slopes. The coastal belt is also where complex processes of sublimation, melt and refreezing occur. Thus, high-resolution modelling is necessary to adequately capture the effects of small-scale variations in topography on the atmospheric variables in this area, but limitations in computing resources prevent such resolution at the scale of Antarctica in full climate models. We present here a downscaling method leading to 15-km SMB resolution for century time-scales over Antarctica. We compute the effect of the fine topography on orographic precipitation and on boundary layer processes that lead to sublimation, melt and refreezing. We first display the SMB downscaled from ERA-Interim and show that the downscaling improves the agreement between modelled and observed SMB for the end of the 20th century. We then present hi-resolution features of the Antarctic SMB evolution during the 21st century downscaled from LMDZ4 for different scenarios. We show that a higher resolution induce at the same time more run-off but a significantly higher mitigation of sea level rise. |
format |
Conference Object |
author |
Agosta, Cécile Favier, Vincent Krinner, Gerhard Gallée, Hubert Genthon, Christophe |
author_facet |
Agosta, Cécile Favier, Vincent Krinner, Gerhard Gallée, Hubert Genthon, Christophe |
author_sort |
Agosta, Cécile |
title |
Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
title_short |
Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
title_full |
Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
title_fullStr |
Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
title_full_unstemmed |
Evolution of the Antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
title_sort |
evolution of the antarctic surface mass balance by high-resolution downscaling and impact on sea-level change for the next centuries |
publishDate |
2012 |
url |
https://orbi.uliege.be/handle/2268/145011 https://orbi.uliege.be/bitstream/2268/145011/1/SCAR-2012.pdf |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_source |
XXXII SCAR and Open Science Conference, Portland, Oregon, United States [US], du 13 au 19 juillet 2012 |
op_relation |
https://orbi.uliege.be/handle/2268/145011 info:hdl:2268/145011 https://orbi.uliege.be/bitstream/2268/145011/1/SCAR-2012.pdf |
op_rights |
open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess |
_version_ |
1796947623476723712 |