Mechanism of Monsoon involves the following concept: The phenomena of monsoon refer to the seasonal reversal of winds. It is because while the South West Monsoon winds blow from sea to land at the end of the summer season, the North east winds blow from land to sea during the winter season.

The differential heating and cooling of land and water creates low pressure on the landmass of India while the seas around experience comparatively high pressure.

The differential heating and cooling of land and water create low pressure on the land of India while the Seasons around experience comparatively high pressure the shift of the position of intertropical convex zone it ITCZ in summer take Ganga plane this is equatorial through normally positioned about 5 degree north of the equator it is also known as the monsoon through during the monsoon season the pressure of the high pressure area east of midcaster approximately at 20 degree South Over the Indian Ocean the intensity and position of this high pressure area affect the Indian monsoon the Tibetan plate instancely heated during summer with results in strong vertical aircurrent and the formation of low pressure over the plateau and about a kilometre about the sea level the movement of the victory to the north of the Himalayas and the pressure of the Tropical easterly that stream over the Indian Peninsular during summer