What are the characteristics of tropical monsoon climate?

Tropical monsoon climate is a climate type, characterized by high temperature all the year round, with the annual average temperature above 22 degrees Celsius, and the Leng Yue is basically above 18 degrees Celsius. The wet and dry seasons are obvious, the precipitation is concentrated in the rainy season, and the precipitation is large, the monsoon is obvious, and tropical cyclones prevail. The tropical monsoon climate is mainly distributed in Southeast Asia from north latitude 10 degrees to the Tropic of Cancer.

Under the control of the dry northeast monsoon, there is little precipitation in winter, and the temperature is the coolest moment of the year. Generally, the average humidity is often between 50% and 75%, which is a dry and cool dry season.

The summer half-year is the hottest half-year in a year, because the sun in the northern hemisphere has begun to get warmer. After the arrival of the southwest monsoon, it is easy to produce various stagnation fronts, such as tropical cyclones produced by the ocean and thunderstorms caused by thermal convection in the afternoon. Rainfall has increased significantly, with occasional heavy rain. At this time, the average humidity generally falls between 75~ 100%, which makes people feel unbearable humidity.

Climatic causes of tropical monsoon;

In the dry season, influenced by the northeast trade wind and the northeast monsoon blowing from the inland of Asia to the ocean and deflecting at low latitudes, the positions of the pressure belt and the wind belt move southward.

In the rainy season, due to the northward movement of the pressure belt and wind belt in summer, this area is affected by the southwest monsoon caused by the deflection of the southeast trade wind across the equator and the monsoon blowing from the ocean to the land caused by the difference in thermal properties between land and sea.