monsoons increase

Despite weakening of the dynamical monsoon circulation, atmospheric buildup due to increased greenhouse gases and consequent temperature increase results in a larger moisture flux and more precipitation for the Indian monsoon. (Douville et al 2000, IPCC 2001, Ashrit et al 2003, Meehl and Arblaster 2003, May 2004, Ashrit et al 2005) IPCC: Climate Change 2007: Working Group 1: The Physical Science Basis 10.3.5.2 Monsoons
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