Japan Geoscience Union Meeting 2018

Presentation information

[EJ] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS06] Global climate change driven by the Southern Ocean and the Antarctic Ice Sheet

Mon. May 21, 2018 3:30 PM - 5:00 PM 302 (3F International Conference Hall, Makuhari Messe)

convener:Osamu Seki(Institute of Low Temperature Science, Hokkaido University), Akira Oka(Atmosphere and Ocean Research Institute, The University of Tokyo), Ryosuke Makabe(国立極地研究所, 共同), Ryu Uemura(University of the Ryukyus), Chairperson:Fukuda Yoichi(Kyoto University), Oyabu Ikumi(National Institute of Polar Research)

3:30 PM - 3:45 PM

[MIS06-12] Response of the Antarctic ice sheet to increased sub-ice-shelf melt rates

*Ralf Greve1, Fuyuki SAITO2, Shun Tsutaki3, Takashi Obase3, Ayako Abe-Ouchi3 (1.Institute of Low Temperature Science, Hokkaido University, 2.Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 3.Atmosphere and Ocean Research Institute, University of Tokyo)

Keywords:Antarctica, Ice sheet, Ice shelf, Basal melting, Climate change, Modelling

The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) brings together a consortium of international ice sheet and climate models to explore the contribution from the Greenland and Antarctic ice sheets to future sea level rise (SLR). LARMIP (Linear Antarctic Response Model Intercomparison Project) and ABUMIP (Antarctic Buttressing Model Intercomparison Project) are initiatives within ISMIP6 to explore the sensitivity of the Antarctic ice sheet to increased basal melting rates under the ice shelves, which was identified as the process to which the ice sheet is likely most vulnerable by the SeaRISE project (Bindschadler et al. 2013, J. Glaciol. 59, 195-224). We contribute to LARMIP and ABUMIP with the ice sheet model SICOPOLIS, thus investigating the effect of the full range from moderately increased basal melting rates to extreme scenarios that melt away all floating ice rapidly. As shown in the figure, over the next 200 years, the mass loss of the ice sheet (contribution to SLR) depends approximately linearly on the melting-rate increase up to ~4 m/a, while for larger melting rates, some saturation shows up (sub-linear response). An extreme scenario with 400 m/a basal melting removes almost all floating ice within a few years, which leads to contributions to SLR of ~0.7 metres after 100 years and ~1.2 metres after 200 years. The sensitivity to regionally increased basal melting rates (region definitions by LARMIP) decreases in the order Weddell > East Antarctica > Ross > Amundsen > Antarctic Peninsula.