q 2000 American Meteorological Society Antarctic Sea Ice Extent Variability and Its Global Connectivity*

• Main Authors: Xiaojun Yuan, Douglas, G. Martinson
• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Published: 1997
• Subjects: Amundsen Sea; Antarctic; Bellingshausen Sea; Drake Passage; Indian; Pacific; The Antarctic; Weddell; Antarc*; Sea ice
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.4499; http://www.ldeo.columbia.edu/res/div/ocp/pub/yuan/2000JC_Yuan.pdf

This study statistically evaluates the relationship between Antarctic sea ice extent and global climate variability. Temporal cross correlations between detrended Antarctic sea ice edge (SIE) anomaly and various climate indices are calculated. For the sea surface temperature (SST) in the eastern equatorial Pacific and tropical Indian Ocean, as well as the tropical Pacific precipitation, a coherent propagating pattern is clearly evident in all correlations with the spatially averaged (over 128 longitude) detrended SIE anomalies (^SIE*&). Correlations with ENSO indices imply that up to 34 % of the variance in ^SIE* & is linearly related to ENSO. The ^SIE* & has even higher correlations with the tropical Pacific precipitation and SST in the tropical Indian Ocean. In addition, correlation of ^SIE* & with global surface temperature produces four characteristic correlation patterns: 1) an ENSO-like pattern in the Tropics with strong correlations in the Indian Ocean and North America (r. 0.6); 2) a telecon-nection pattern between the eastern Pacific region of the Antarctic and western–central tropical Pacific; 3) an Antarctic dipole across the Drake Passage; and 4) meridional banding structures in the central Pacific and Atlantic expending from polar regions to the Tropics, even to the Northern Hemisphere. The SIE anomalies in the Amundsen Sea, Bellingshausen Sea, and Weddell Gyre of the Antarctic polar ocean sectors show the strongest polar links to extrapolar climate. Linear correlations between ^SIE* & in those regions