The Winter (NORTH EAST) Monsoon

Gap-fill exercise

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Look carefully at the relevant diagram first!

During the northern hemisphere , the overhead sun, the ITCZ and the sub-tropical jet all move southwards. At the same time, central experiences intense cooling which allows a large pressure system to develop. Airstreams which move outwards from this high pressure area will be because their source area is semi-desert.

They will become even drier as they cross the and adiabatically warmer as they descend to the Indo-Gangetic . Mumbai receives less than 100mm of rain during these 8 months.

The monsoon, which in reality is much more complex than this model described here, affects one of the world's population. Unfortunately, monsoon rainfall, especially in the Indian sub-continent, is unreliable. If the rains fail, then and famine will ensue. 1987 was the ninth year in a decade when the monsoon failed to arrive in north-west India. If, conversely there is excessive rainfall then large areas of land experience extreme such as Bangladesh (1998, 2002 and in many other years).