A historical bias metric was computed, incorporating atmosphere and.

Lipscomb 6, Ayako Abe-Ouchi 7, Ccile Agosta 8, Torsten Albrecht 9, Xylar Asay-Davis 10, Alice Barthel 10, Reinhard Calov 9, Richard Cullather 2, Christophe Dumas 8, Benjamin K.

Gregory 13,14, Ralf Greve 15,16, Tore Hattermann 17,18, Matthew J.

Hoffman 10, Angelika Humbert 19,20, Philippe Huybrechts 21, Nicolas C.

Price 10, Aurlien Quiquet 8, Ronja Reese 9, Nicole-Jeanne Schlegel 1, Andrew Shepherd 26, Erika Simon 2, Robin S.

However, there is currently no consensus on estimates of the future mass.

They are forced with outputs from a subset of models from the.

Coupled Model Intercomparison Project Phase 5 (CMIP5), representative of the spread in climate.

Pathway (RCP) 8.5 scenario forcing.

These numbers are relative to a control experiment with.

Amundsen and Bellingshausen sea sectors of West Antarctica and the Antarctic Peninsula have.

Previous modeling studies showed variable Antarctic contribution to sea.

Evolution, Bindschadler et al., 2013; Nowicki et al., 2013 a ) highlighted the large discrepancies in numerical ice.

ISMIP6 (Ice Sheet Model Intercomparison Project for CMIP6, Nowicki et al., 2016 ) is the primary.

Antarctic experiments were based on simplified forcings: the surface mass.

AtmosphereOcean General Circulation Models (AOGCMs), including both Climate Models and Earth System Models.

Pathway (RCP) scenarios, ocean-induced melt parameterizations and simulated physical processes on.

Sect. 3. Section 4 analyzes the results and assesses the impact of the different scenarios and.

In this section, we summarize the experimental protocol for ISMIP6-Antarctica projections, including.

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