Abstract
In order to assess the impact of the mid-tropospheric
circulation over the Greenland ice sheet (GrIS)
on surface melt, as simulated by the regional climate model
MAR, an automatic Circulation type classification (CTC)
based on 500 hPa geopotential height from reanalyses is
developed. General circulation correlates significantly with
the surface melt anomalies for the summers in the period
1958–2009. The record surface melt events observed during
the summers of 2007–2009 are linked to the exceptional
persistence of atmospheric circulations favouring
warm air advection. The CTC emphasizes that summer
500 hPa circulation patterns have changed since the
beginning of the 2000s; this process is partly responsible
for the recent warming observed over the GrIS
Original language | English |
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Pages (from-to) | 139-159 |
Number of pages | 21 |
Journal | Climate Dynamics |
Volume | 36 |
DOIs | |
Publication status | Published - 2010 |