Spatial and temporal Antarctic Ice Sheet mass trends, glacio-isostatic adjustment, and surface processes from a joint inversion of satellite altimeter, gravity, and GPS data.

J Geophys Res Earth Surf · 2016 · PMC4845667 · PMID 27134805

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a positive trendno p-value reported

The total mass loss is partly compensated by a significant mass gain of 56 ± 18 Gt yr −1 in East Antarctica due to a positive trend of surface mass balance anomalies.

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