monsoons decrease

………………………………….

We have presented evidence from observations that the equitorial Indian Ocean has warmed by about 0.6 to 0.8K during 1950 to 2002, accompanied by a dramatic weakening of the summertime SST gradient in the NIO.

In the model, the weakening of the meridional NIO_SST gradient leads to a large decrease in Indian rainfall during summer months, ranging form 2 to 3 mm per day. Reduction in the NIO_SST gradient basically weakens the model monsoonal circulation and shifts model rainfall from India to sub-Saharan Africa.

Chul Eddy Chung and V. Ramanthan, American Meteorological Society, Journal of Climate, Vol19 Issue 10 (May 2006)