Japan Geoscience Union Meeting 2021

Presentation information

[E] Poster

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS05] Global climate change driven by the Southern Ocean and the Antarctic Ice Sheet

Sun. Jun 6, 2021 5:15 PM - 6:30 PM Ch.20

convener:Osamu Seki(Institute of Low Temperature Science, Hokkaido University), Yoshifumi Nogi(National Institute of Polar Research), Akira Oka(Atmosphere and Ocean Research Institute, The University of Tokyo), Yusuke Suganuma(National institute of Polar Research)

5:15 PM - 6:30 PM

[MIS05-P16] A linkage between Antarctic sea-ice extent and ice-shelf basal melting in summer: A circumpolar model study

*Kazuya Kusahara1 (1.Japan Agency for Marine-Earth Science and Technology)

Keywords:ice shelf-ocean interaction, sea ice

Recent observations indicate that two cryospheric components, namely the Antarctic sea ice and ice shelf over the Southern Ocean, have been changing over the decades. Here we analyze results from an ocean–sea ice–ice shelf model to examine the relationship between the Antarctic sea-ice extent and ice-shelf basal melting. The model reproduces seasonal and interannual variability in the Antarctic sea-ice extent and indicates that summertime ice-shelf basal melting is closely anti-correlated with the sea-ice extent anomaly. For example, the unprecedented minimum of the Antarctic sea-ice extent in the 2016 spring was accompanied by a substantial increase in the Antarctic ice-shelf melting in the model. Detailed analysis of Antarctic coastal water masses flowing into the ice-shelf cavities reveals a possible physical link in the strong anti-correlation. This study suggests that the Antarctic sea-ice extent in summer can be a proxy for Antarctic coastal water masses and subsequent ice-shelf melting.