Acceleration of dynamic ice loss in Antarctica from satellite gravimetry

Theresa Diener (1, 2) , Ingo Sasgen (2) , Cécile Agosta (3, 4) , Johannes J. Fürst (1) , Matthias H. Braun (1) , Hannes Konrad (5) , Xavier Fettweis (6)

1 FAU - Friedrich-Alexander Universität Erlangen-Nürnberg = University of Erlangen-Nuremberg
2 AWI - Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine
3 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
4 GLACCIOS - Glaces et Continents, Climats et Isotopes Stables
5 DWD - Deutscher Wetterdienst [Offenbach]
6 Université de Liège

The dynamic stability of the Antarctic Ice Sheet is one of the largest uncertainties in projections of future global sea-level rise. Essential for improving projections of the ice sheet evolution is the understanding of the ongoing trends and accelerations of mass loss in the context of ice dynamics. Here, we examine accelerations of mass change of the Antarctic Ice Sheet from 2002 to 2020 using data from the GRACE (Gravity Recovery and Climate Experiment; 2002-2017) and its follow-on GRACE-FO (2018-present) satellite missions. By subtracting estimates of net snow accumulation provided by re-analysis data and regional climate models from GRACE/GRACE-FO mass changes, we isolate variations in ice-dynamic discharge and compare them to direct measurements based on the remote sensing of the surface-ice velocity (2002-2017). We show that variations in the GRACE/GRACE-FO time series are modulated by variations in regional snow accumulation caused by large-scale atmospheric circulation. We show for the first time that, after removal of these surface effects, accelerations of ice-dynamic discharge from GRACE/GRACE-FO agree well with those independently derived from surface-ice velocities. For 2002-2020, we recover a discharge acceleration of-5.3 ± 2.2 Gt yr$^{−2}$ for the entire ice sheet; these increasing losses originate mainly in the Amundsen and Bellingshausen Sea Embayment regions (68%), with additional significant contributions from Dronning Maud Land (18%) and the Filchner-Ronne Ice Shelf region (13%). Under the assumption that the recovered rates and accelerations of mass loss persisted independent of any external forcing, Antarctica would contribute 7.6 ± 2.9 cm to global mean sea-level rise by the year 2100, more than two times the amount of 2.9 ± 0.6 cm obtained by linear extrapolation of current GRACE/GRACE-FO mass loss trends.

Mots clés: Antarctica; GRACE/GRACE-FO; ice-dynamic discharge; surface mass balance; sea-level rise (SLR); mass balance; ISMIP6; climate indices

Domaines: Océan, Atmosphère; Interfaces continentales, environnement

Theresa Diener, Ingo Sasgen, Cécile Agosta, Johannes J. Fürst, Matthias H. Braun, et al.. Acceleration of dynamic ice loss in Antarctica from satellite gravimetry. Frontiers in Earth Science, 2021, 9, pp.741789. ⟨10.3389/feart.2021.741789⟩. ⟨hal-03510587⟩