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T. N. Krishnamurti

condensation heating and it follows the course of this maximum rainfall belt. The behavior of the monsoon overIndia is largely dictated by the differential heating between the principal region of rainfall and a net coolingin the surrounding regions. The location of the axis ofdifferential heating can usually be approximated fromthe regions of divergent inflows to the divergent outflows at the 200 mb surface. The mode of migrationof the region of heating from northern Burma in themonth of May to the

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