The primary cause of monsoon is the seasonal reversal of winds. Understanding the mechanism can be broken down into a few key concepts:
Monsoon winds are a result of the larger scale wind patterns that reverse direction with the changes in seasons. This primarily occurs due to differential heating.
During the summer, the land heats up more quickly than the ocean, creating a low-pressure zone over the land. In contrast, a high-pressure zone forms over the cooler ocean.
This pressure difference causes wind to flow from the high-pressure area (ocean) towards the low-pressure area (land), bringing with it moist air which results in precipitation.
During the winter, the situation reverses with the ocean maintaining a higher temperature than the land, changing the direction of winds. Therefore, in places like South Asia, the monsoon is characterized by the inflow of moisture-laden winds in the summer and dry winds in the winter.