Precambrian ultramafic rocks south of Sermilik, Frederikshåb district, South-West Greenland
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چکیده
منابع مشابه
Dark ice dynamics of the south-west Greenland Ice Sheet
Runoff from the Greenland Ice Sheet (GrIS) has increased in recent years due largely to changes in atmospheric circulation and atmospheric warming. Albedo reductions resulting from these changes have amplified surface melting. Some of the largest declines in GrIS albedo have occurred in the ablation zone of the south-west sector and are associated with the development of “dark” ice surfaces. Fi...
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ژورنال
عنوان ژورنال: Bulletin Grønlands Geologiske Undersøgelse
سال: 1973
ISSN: 2597-2936,0105-3507
DOI: 10.34194/bullggu.v107.6648