The instrumental record of Antarctic sea ice in recent decades does not reveal a clear signature of warming despite observational evidence from coastal Antarctica. Here we report a significant correlation (P < 0.002) between methanesulphonic acid (MSA) concentrations from a Law Dome ice core and 22 years of satellite-derived sea ice extent (SIE) for the 80°E to 140°E sector. Applying this instrumental calibration to longer term MSA data (1841 to 1995 A.D.) suggests that there has been a 20% decline in SIE since about 1950. The decline is not uniform, showing large cyclical variations, with periods of about 11 years, that confuse trend detection over the relatively short satellite era.
History
Publication title
Science
Volume
302
Issue
5648
Pagination
1203-1206
ISSN
0036-8075
Department/School
Institute for Marine and Antarctic Studies
Publisher
American Association Advancement Science
Place of publication
Washington, USA
Rights statement
Copyright 2003 The Authors
Repository Status
Restricted
Socio-economic Objectives
Other environmental management not elsewhere classified