The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation

With the aim to study the impact of the mid-tropospheric circulation on the Greenland ice sheet (GrIS) surface melt simulated by the regional climate model MAR, we developed an automatic Circulation Type Classification (CTC) based on the 500hPa geopotential height from reanalyses over the period 195...

Full description

Bibliographic Details
Main Author: Fettweis, Xavier
Format: Conference Object
Language:English
Published: 2009
Subjects:
Online Access:https://orbi.uliege.be/handle/2268/36762
https://orbi.uliege.be/bitstream/2268/36762/1/Fettweis-2009-EGU-Talk.pdf
id ftorbi:oai:orbi.ulg.ac.be:2268/36762
record_format openpolar
spelling ftorbi:oai:orbi.ulg.ac.be:2268/36762 2024-04-21T08:03:26+00:00 The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation Fettweis, Xavier 2009-04-23 https://orbi.uliege.be/handle/2268/36762 https://orbi.uliege.be/bitstream/2268/36762/1/Fettweis-2009-EGU-Talk.pdf en eng http://meetingorganizer.copernicus.org/EGU2009/EGU2009-7855.pdf https://orbi.uliege.be/handle/2268/36762 info:hdl:2268/36762 https://orbi.uliege.be/bitstream/2268/36762/1/Fettweis-2009-EGU-Talk.pdf open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess EGU General Assembly 2009, Vienna, Austria [AT] 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 2009 ftorbi 2024-03-27T14:43:04Z With the aim to study the impact of the mid-tropospheric circulation on the Greenland ice sheet (GrIS) surface melt simulated by the regional climate model MAR, we developed an automatic Circulation Type Classification (CTC) based on the 500hPa geopotential height from reanalyses over the period 1958-2008. This CTC shows that the dominant mode of the regional atmospheric summer variability around the GrIS is linked to the North Atlantic Oscillation (NAO) and that the surface melt anomalies are highly correlated to the general circulation. It explains notably why a record surface melt was observed during the summers 2007 and 2008. In addition, the climate conditions occurring the 27th August of 2003, where the GrIS temperature was 10°C higher than the normal, were the consequence of an almost unique 500 hPa circulation in the 50 last years. Conference Object Greenland Ice Sheet North Atlantic North Atlantic oscillation 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
Fettweis, Xavier
The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
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 With the aim to study the impact of the mid-tropospheric circulation on the Greenland ice sheet (GrIS) surface melt simulated by the regional climate model MAR, we developed an automatic Circulation Type Classification (CTC) based on the 500hPa geopotential height from reanalyses over the period 1958-2008. This CTC shows that the dominant mode of the regional atmospheric summer variability around the GrIS is linked to the North Atlantic Oscillation (NAO) and that the surface melt anomalies are highly correlated to the general circulation. It explains notably why a record surface melt was observed during the summers 2007 and 2008. In addition, the climate conditions occurring the 27th August of 2003, where the GrIS temperature was 10°C higher than the normal, were the consequence of an almost unique 500 hPa circulation in the 50 last years.
format Conference Object
author Fettweis, Xavier
author_facet Fettweis, Xavier
author_sort Fettweis, Xavier
title The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
title_short The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
title_full The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
title_fullStr The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
title_full_unstemmed The 1958-2008 Greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
title_sort 1958-2008 greenland ice sheet surface melt and the mid-tropospheric atmospheric circulation
publishDate 2009
url https://orbi.uliege.be/handle/2268/36762
https://orbi.uliege.be/bitstream/2268/36762/1/Fettweis-2009-EGU-Talk.pdf
genre Greenland
Ice Sheet
North Atlantic
North Atlantic oscillation
genre_facet Greenland
Ice Sheet
North Atlantic
North Atlantic oscillation
op_source EGU General Assembly 2009, Vienna, Austria [AT]
op_relation http://meetingorganizer.copernicus.org/EGU2009/EGU2009-7855.pdf
https://orbi.uliege.be/handle/2268/36762
info:hdl:2268/36762
https://orbi.uliege.be/bitstream/2268/36762/1/Fettweis-2009-EGU-Talk.pdf
op_rights open access
http://purl.org/coar/access_right/c_abf2
info:eu-repo/semantics/openAccess
_version_ 1796943278300463104