Affiliation:
1. Earth and Life Institute Université catholique de Louvain Louvain‐la‐Neuve Belgium
2. Ice Dynamics and Paleoclimate British Antarctic Survey Cambridge UK
Abstract
AbstractSea‐ice extent is predicted to decrease in a warming climate. However, despite global warming over the past century, total Antarctic sea ice remained relatively stable from 1979 until 2015, before strongly melting. Here we explore the long‐term sea ice variability by reconstructing Antarctic sea ice since 1700 CE, based on paleoclimate records and data assimilation. Our results indicate a decline in southern hemisphere sea‐ice extent over the 20th century, driven by a reduction of 0.26 million km2 in the Weddell Sea that reached values at the end of the century lower than any other reconstructed period. The Ross Sea experienced an increasing sea‐ice cover trend due to a low‐pressure system located off the Amundsen Sea coast, offset by a decreasing trend in the Bellingshausen‐Amundsen Sea. Models failed to account for the Ross Sea increase, resulting in an overly uniform estimate of Antarctic sea ice loss over the 20th century.
Funder
Fonds De La Recherche Scientifique - FNRS
Belgian Federal Science Policy Office
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics