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GEOPHYSICAL RESEARCH LETTERS,
VOL. 31,
L24206,
doi:10.1029/2004GL021473,
2004
Sea-surface temperature induced variability of the Southern Annular Mode in an atmospheric general circulation model
Tianjun Zhou
State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric
Physics, Chinese Academy of Sciences, Beijing, China
Rucong Yu
State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric
Physics, Chinese Academy of Sciences, Beijing, China
Abstract
The reproducibility of the Southern Hemisphere Annular Mode (SAM) is examined by using the NCAR CAM2 model forced with historical
sea surface temperature covering the time period of 1950–2000. There is some correspondence (low however significant correlation)
between the simulation and observation in the temporal evolution of the SAM, indicating if global SSTs are known and prescribed
to the model, there would be some predictability to the SAM. The reproducibility is greater during austral summer than winter,
and the source of much of the reproducibility is tropical Pacific SST, with equatorial Pacific warm event corresponds to a
negative phase SAM in austral summer. There is a hint that this result is model independent. Working with ensembles improves
the reproducibility.
Received 13
September
2004;
accepted 19
November
2004;
published 22
December
2004.
Index Terms: 1620 Global Change: Climate dynamics (3309); 1610 Global Change: Atmosphere (0315, 0325); 3319 Meteorology and Atmospheric Dynamics: General circulation; 3339 Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions (0312, 4504); 3334 Meteorology and Atmospheric Dynamics: Middle atmosphere dynamics (0341, 0342).
Read Full Article (file size: 731987 bytes) Cited by
Citation: Zhou, T., and R. Yu
(2004),
Sea-surface temperature induced variability of the Southern Annular Mode in an atmospheric general circulation model,
Geophys. Res. Lett.,
31,
L24206,
doi:10.1029/2004GL021473.
Copyright 2004 by the American Geophysical Union.
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