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GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L21305, doi:10.1029/2004GL021169, 2004

Changes in the ocean transport through Drake Passage during the 1980s and 1990s, forced by changes in the Southern Annular Mode

Michael P. Meredith

Proudman Oceanographic Laboratory, Bidston Observatory, Wirral, UK


Philip L. Woodworth

Proudman Oceanographic Laboratory, Bidston Observatory, Wirral, UK


Chris W. Hughes

Proudman Oceanographic Laboratory, Bidston Observatory, Wirral, UK


Vladimir Stepanov

Proudman Oceanographic Laboratory, Bidston Observatory, Wirral, UK


Abstract

We present the first direct evidence that interannual changes in ocean transport through Drake Passage are forced by variability in the Southern Annular Mode (SAM). This evidence is derived from two decades (1980s and 1990s) of subsurface pressure measurements from the tide gauge at Faraday station (western Antarctic Peninsula), combined with the output of an ocean general circulation model. In recent decades, the SAM has moved toward a higher-index state (stronger circumpolar winds); this trend is not simply monotonic, but is the product of a long-term change in the seasonality of the SAM. Whilst we cannot address directly the effect of the long-term trend on circumpolar transport, bottom pressure data from Drake Passage during the 1990s demonstrate that ocean transport showed the same changes in seasonality as did the SAM. This offers a mechanism for atmospheric climate change to influence directly the large-scale ocean circulation.

Received 1 August 2004; accepted 14 October 2004; published 6 November 2004.

Index Terms: 4207 Oceanography: General: Arctic and Antarctic oceanography; 4215 Oceanography: General: Climate and interannual variability (3309); 4532 Oceanography: Physical: General circulation; 1635 Global Change: Oceans (4203); 4556 Oceanography: Physical: Sea level variations.

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Citation: Meredith, M. P., P. L. Woodworth, C. W. Hughes, and V. Stepanov (2004), Changes in the ocean transport through Drake Passage during the 1980s and 1990s, forced by changes in the Southern Annular Mode, Geophys. Res. Lett., 31, L21305, doi:10.1029/2004GL021169.