Reference : Greenland [in "State of the Climate in 2008"]
Scientific journals : Article
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
http://hdl.handle.net/2268/36758
Greenland [in "State of the Climate in 2008"]
English
Box, J. [> >]
Bai, L. [> >]
Benson, R. [> >]
Bhattacharya, I. [> >]
Bromwich, D. [> >]
Cappelen, J. [> >]
Decker, D. [> >]
DiGirolamo, N. [> >]
Fettweis, Xavier mailto [Université de Liège - ULg > Département de géographie > Topoclimatologie >]
Hall, D. [> >]
Hanna, E. [> >]
Mote, T. [> >]
Tedesco, M. [> >]
van de Wal, R. [> >]
van den Broeke, M. [> >]
2009
Bulletin of the American Meteorological Society (BAMS)
90
108-112
Yes (verified by ORBi)
International
0003-0007
[en] An abnormally cold winter across the southern half of Greenland led to substantially higher west coast sea ice thickness and concentration. Even so, record-setting summer temperatures around Greenland, combined with an intense melt season (particularly across the northern ice sheet), led the 2008 Greenland climate to be marked by continued ice sheet mass deficit and floating ice disintegration.
http://hdl.handle.net/2268/36758
http://www.ncdc.noaa.gov/oa/climate/research/2008/ann/bams/

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