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GEOPHYSICAL RESEARCH LETTERS,
VOL. 32,
L11603,
doi:10.1029/2005GL022727,
2005
Impact of the Southern Annular Mode on Southern Ocean circulation and biology
Nicole S. Lovenduski
Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, California, USA
Nicolas Gruber
Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, California, USA
Abstract
We investigate the impact of the Southern Annular Mode (SAM) on surface wind, sea surface temperature (SST), and surface chlorophyll
concentration on intraseasonal to interannual timescales in the Southern Ocean using 8-day average satellite observations.
Positive phases of the SAM are associated with enhanced westerly winds over the Antarctic Zone (AZ) and Polar Frontal Zone,
driving increased equatorward Ekman transport and cold SST anomalies in these regions. Positive SAM is also associated with
easterly wind and warm SST anomalies in the Subtropical Zone. South of the Antarctic Polar Front (APF), chlorophyll concentration
anomalies are positively correlated with the SAM, however this correlation is negative north of the APF. We suggest that the
positive correlation in the AZ is due to the increased supply of iron by upwelling, while the negative correlation north of
the APF is caused by stronger light limitation as a consequence of deeper mixed layers.
Received 15
February
2005;
accepted 5
May
2005;
published 8
June
2005.
Index Terms: 4215 Oceanography: General: Climate and interannual variability (1616, 1635, 3305, 3309, 4513); 4273 Oceanography: General: Physical and biogeochemical interactions; 4275 Oceanography: General: Remote sensing and electromagnetic processes (0689, 2487, 3285, 4455, 6934); 4806 Oceanography: Biological and Chemical: Carbon cycling (0428).
Read Full Article (file size: 267342 bytes) Cited by
Citation: Lovenduski, N. S., and N. Gruber
(2005),
Impact of the Southern Annular Mode on Southern Ocean circulation and biology,
Geophys. Res. Lett.,
32,
L11603,
doi:10.1029/2005GL022727.
Copyright 2005 by the American Geophysical Union.
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