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

• Main Authors: Martin-Espanol, A, Zammit-Mangion, A, Clarke, PJ, Flament, T, Helm, V, Matt King, Luthcke, SB, Petrie, E, Remy, F, Schon, N, Wouters, B, Bamber, JL
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2016
• Subjects: Geodesy; Satellite-based positioning; glacial isostatic adjustment; GPS; Antarctica; ice; Amundsen Sea; Antarctic; Antarctic Peninsula; East Antarctica; The Antarctic; West Antarctica; Antarc*; Ice Sheet
• Online Access: https://figshare.com/articles/journal_contribution/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/22935101

We present spatiotemporal mass balance trends for the Antarctic Ice Sheet from a statistical inversion of satellite altimetry, gravimetry, and elastic-corrected GPS data for the period 2003–2013. Our method simultaneously determines annual trends in ice dynamics, surface mass balance anomalies, and a time-invariant solution for glacio-isostatic adjustment while remaining largely independent of forward models. We establish that over the period 2003–2013, Antarctica has been losing mass at a rate of −84 ± 22 Gt yr −1 , with a sustained negative mean trend of dynamic imbalance of −111 ± 13 Gt yr −1 . West Antarctica is the largest contributor with −112 ± 10 Gt yr −1 , mainly triggered by high thinning rates of glaciers draining into the Amundsen Sea Embayment. The Antarctic Peninsula has experienced a dramatic increase in mass loss in the last decade, with a mean rate of −28 ± 7 Gt yr −1 and significantly higher values for the most recent years following the destabilization of the Southern Antarctic Peninsula around 2010. 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.