Tropical Monsoon Definition ((install)) -

Tropical monsoons are caused by the uneven heating of land and sea during the summer months. As the land heats up, it warms faster than the sea, creating a temperature gradient. This temperature difference causes the winds to blow from the ocean to the land, bringing moist air and resulting in heavy rainfall.

The defining feature of this climate is the reversal of wind directions (monsoons), which causes a sharp contrast in precipitation: tropical monsoon definition

Still confused? Here is the cheat sheet: Tropical monsoons are caused by the uneven heating

To be classified under this definition, a region must meet several strict meteorological criteria: The defining feature of this climate is the

This is the "Tropical" part. You will never need a snow shovel. Average monthly temperatures stay above 64°F (18°C) every single month.

"Monsoon" actually comes from the Arabic word mausim , meaning "season." For half the year, winds blow (bringing moisture). For the other half, winds blow from the land (bringing dust and dry air).