Thermal tracking of meltwater retention in Greenland's accumulation area

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Thermal tracing of retained meltwater in the lower accumulation area of the Southwestern Greenland ice sheet

We present in situ firn temperatures from the extreme 2012 melt season in the southwestern lower accumulation area of the Greenland ice sheet. The upper 2.5 m of snow and firn was temperate during the melt season, when vertical meltwater percolation was inefficient due to a 5.5 m thick ice layer underlying the temperate firn. Meltwater percolation and refreezing beneath 2.5 m depth only occurre...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Earth Surface

سال: 2012

ISSN: 0148-0227

DOI: 10.1029/2011jf002083