|
Read Full Article Cited by
GEOPHYSICAL RESEARCH LETTERS,
VOL. 28, NO. 19,
PAGES 3717–3720,
2001
January 1999 Indian Ocean Cooling Event
D. E. Harrison
Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle
Gabriel A. Vecchi
Department of Atmospheric Sciences, University of Washington, Seattle
Abstract
Unexpectedly strong sub-seasonal SST variability over the tropical Indian Ocean has been observed by the TRMM microwave imager,
which provides unprecedented tropical SST information in the presence of clouds. In January-February 1999 SST averaged over
an area 20° longitude by 10° latitude cooled by ∼1.5°C over 10 days and warmed by ∼1.25°C in the following week. Local changes
were up to ±3°C. There were strong variations in atmospheric convection and surface wind stress associated with the SST variability.
The evolution of the convection suggests a feedback from the SST changes into atmospheric convection. Net air-sea heat-flux
cannot account for the observed cooling; oceanic processes are fundamental to this event. The roles of such sub-seasonal ocean-atmosphere
interactions in the evolution of the Madden-Julian Oscillation, the seasonal and the interannual variability of Indian Ocean
SST deserve further investigation.
Received 11
May
2001;
accepted 16
July
2001.
Read Full Article Cited by
Citation: Harrison, D. E., and G. A. Vecchi
(2001),
January 1999 Indian Ocean Cooling Event,
Geophys. Res. Lett.,
28(19),
3717–3720.
Copyright 2001 by the American Geophysical Union.
|