Reference : Current and future atmospheric circulation at 500 hPa over Greenland simulated by the CM...
Scientific journals : Article
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
http://hdl.handle.net/2268/131762
Current and future atmospheric circulation at 500 hPa over Greenland simulated by the CMIP3 and CMIP5 global models
English
Belleflamme, Alexandre mailto [Université de Liège - ULg > Département de géographie > Topoclimatologie >]
Fettweis, Xavier mailto [Université de Liège - ULg > Département de géographie > Topoclimatologie >]
Lang, Charlotte [Université de Liège - ULg > Département de géographie > Topoclimatologie >]
Erpicum, Michel mailto [Université de Liège - ULg > Département de géographie > Topoclimatologie >]
2013
Climate Dynamics
Springer
41
7-8
Yes (verified by ORBi)
International
0930-7575
Berlin Heidelberg
Allemagne
[en] General circulation models ; 500 hPa geopotential height ; Greenland ; Circulation type classification
[en] The Greenland ice sheet is projected to be strongly affected by global warming. These projections are either issued from downscaling methods (such as Regional Climate Models) or they come directly from General Circulation Models (GCMs). In this context, it is necessary to evaluate the accuracy of the daily atmospheric circulation simulated by the GCMs, since it is used as forcing for downscaling methods. Thus, we use an automatic circulation type classification based on two indices (Euclidean distance and Spearman rank correlation using the daily 500 hPa geopotential height) to evaluate the ability of the GCMs from both CMIP3 and CMIP5 databases to simulate the main circulation types over Greenland during summer. For each circulation type, the GCMs are compared to three reanalysis datasets on the basis of their frequency and persistence differences. For the current climate (1961–1990), we show that most of the GCMs do not reproduce the expected frequency and the persistence of the circulation types and that they simulate poorly the observed daily variability of the general circulation. Only a few GCMs can be used as reliable forcings for downscaling methods over Greenland. Finally, when applying the same approach to the future projections of the GCMs, no significant change in the atmospheric circulation over Greenland is detected, besides a generalised increase of the geopotential height due to a uniform warming of the atmosphere.
Researchers
http://hdl.handle.net/2268/131762
10.1007/s00382-012-1538-2
http://www.springerlink.com/content/m765331048634740/
The online version of this article (doi:10.1007/s00382-012-1538-2) contains supplementary
material, which is available to authorized users.

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