Diss us the machanizam of monsons
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Currently , the mechanism of the monsoon is a widely-studied subject globally . In the Indian subcontinent , the mountain barriers to the north guide the flow of the monsoon winds . The Western Ghats , too , play a similar role .
To understand the mechanism of the monsoons . Certain factors have emerged which are taken to be the causes of the wind-reversal .
1) The heat Low around the Arabian sea caused due to intensive heating during the pre-monsoon months .
2) The Northernmost position of inter tropical convergence zone ( ITCZ ) in summer , also known as the monsoon-trough during the monsoon season .
3) High Pressure Indian Ocean . The intensity and position of this high- pressure area affects the Indian monsoon .
4) The Tibetan high-level plateau gets intensely heated during summer , which results in strong vertical air currents and the formation of high pressure over the plateau at about a km above the sea level .
5) The movement of the Westerly jet to the north of the Himalayas and the presence of the tropical Easterly jet over the Indian peninsula during summer .
To understand the mechanism of the monsoons . Certain factors have emerged which are taken to be the causes of the wind-reversal .
1) The heat Low around the Arabian sea caused due to intensive heating during the pre-monsoon months .
2) The Northernmost position of inter tropical convergence zone ( ITCZ ) in summer , also known as the monsoon-trough during the monsoon season .
3) High Pressure Indian Ocean . The intensity and position of this high- pressure area affects the Indian monsoon .
4) The Tibetan high-level plateau gets intensely heated during summer , which results in strong vertical air currents and the formation of high pressure over the plateau at about a km above the sea level .
5) The movement of the Westerly jet to the north of the Himalayas and the presence of the tropical Easterly jet over the Indian peninsula during summer .
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