Title Non-annular atmospheric circulation change induced by stratospheric ozone depletion and its role in the recent increase of Antarctic sea ice extent
Author Turner, J.; Comiso, J.C.; Marshall, G.J.; Lachlan-Cope, T.A.; Bracegirdle, T.; Maksym, T.; Meredith, M.P.; Wang, Z.; Orr, A.
Author Affil Turner, J., British Antarctic Survey, National Environment Research Council, Cambridge, United Kingdom. Other: NASA, Goddard Space Flight Center
Source Geophysical Research Letters, 36(8), Citation L08502. Publisher: American Geophysical Union, Washington, DC, United States. ISSN: 0094-8276
Publication Date 2009
Notes In English. 21 refs. GeoRef Acc. No: 301066. CRREL Acc. No: 64005383
Index Terms atmospheric circulation; ice; microwaves; ozone; remote sensing; Antarctica- -Amundsen Sea; Southern Ocean--Bellingshausen Sea; Southern Ocean--Ross Sea; Amundsen Sea; Antarctica; Bellingshausen Sea; geophysical methods; microwave methods; Ross Sea; satellite methods; sea ice; Southern Ocean
Abstract Based on a new analysis of passive microwave satellite data, we demonstrate that the annual mean extent of Antarctic sea ice has increased at a statistically significant rate of 0.97% dec-1 since the late 1970s. The largest increase has been in autumn when there has been a dipole of significant positive and negative trends in the Ross and Amundsen-Bellingshausen Seas respectively. The autumn increase in the Ross Sea sector is primarily a result of stronger cyclonic atmospheric flow over the Amundsen Sea. Model experiments suggest that the trend towards stronger cyclonic circulation is mainly a result of stratospheric ozone depletion, which has strengthened autumn wind speeds around the continent, deepening the Amundsen Sea Low through flow separation around the high coastal orography. However, statistics derived from a climate model control run suggest that the observed sea ice increase might still be within the range of natural climate variability.
URL http://hdl.handle.net/10.1029/2009GL037524
Publication Type journal article
Record ID 88829