A high resolution record of Greenland mass balance

We map recent Greenland Ice Sheet elevation change at high spatial (5-km) and temporal (monthly) resolution using CryoSat-2 altimetry. After correcting for the impact of changing snowpack properties associated with unprecedented surface melting in 2012, we find good agreement (3 cm/yr bias) with air...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: McMillan, Malcolm, Leeson, Amber Alexandra, Shepherd, Andrew, Briggs, Kate, Armitage, Thomas W. K., Hogg, Anna, Kuipers Munneke, Peter, Van Den Broeke, Michiel, Brice, Noël, van de Berg, Willem Jan, Ligtenberg, Stefan, Horwath, Martin, Groh, Andreas, Muir, Alan, Gilbert, Lin
Format: Article in Journal/Newspaper
Language:English
Published: 2016
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Online Access:https://eprints.lancs.ac.uk/id/eprint/80262/
https://eprints.lancs.ac.uk/id/eprint/80262/1/McMillan_et_al_2016_Geophysical_Research_Letters.pdf
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Summary:We map recent Greenland Ice Sheet elevation change at high spatial (5-km) and temporal (monthly) resolution using CryoSat-2 altimetry. After correcting for the impact of changing snowpack properties associated with unprecedented surface melting in 2012, we find good agreement (3 cm/yr bias) with airborne measurements. With the aid of regional climate and firn modelling, we compute high spatial and temporal resolution records of Greenland mass evolution, which correlate (R = 0.96) with monthly satellite gravimetry, and reveal glacier dynamic imbalance. During 2011-2014, Greenland mass loss averaged 269 ± 51 Gt/yr. Atmospherically-driven losses were widespread, with surface melt variability driving large fluctuations in the annual mass deficit. Terminus regions of five dynamically-thinning glaciers, which constitute less than 1% of Greenland's area, contributed more than 12% of the net ice loss. This high-resolution record demonstrates that mass deficits extending over small spatial and temporal scales have made a relatively large contribution to recent ice sheet imbalance.