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Published byRegina Mertens Modified over 6 years ago
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Pre-Monsoon Monsoon TRMM PR data reveal the nature of the convection producing extreme monsoon rains In the monsoon: Deep cores shift from Bengal to Pakistan Wide mesoscale systems develop along the Himalayan foothills Broad stratiform systems dominate upstream of the mountainous coastlines Deep Convective Cores Wide Convective Cores Broad Stratiform Regions Houze et al. 2007; Romatschke et al. 2010; Romatschke & Houze 2010
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A composite of TRMM PR data in 9 years of hurricanes in the Atlantic basin show that eyewall convection is systematically deeper and more intense than deep convection in the environment of the cyclone Colors represent probability of occurrence with 20, 50, & 80% contours in black. Hence and Houze 2010
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