Traditional Culture Encyclopedia - Weather forecast - What is the tropical monsoon climate?

What is the tropical monsoon climate?

Tropical monsoon climate is a kind of climate type, its main feature is high temperature all year round, and precipitation is divided into dry season and rainy season. It is mainly distributed in the south bank of the Asian continent from 10 to 23 26 north latitude, and it is a unique climate in Asia. It is distributed in China, Guangdong Leizhou Peninsula, Hainan Island, South China Sea, South Island of Taiwan Province Province, Indo-China Peninsula (north of central Malay Peninsula), northern Philippine Islands, South Asia and other regions, that is, the South Asian monsoon region.

Climatic characteristics:

1, the temperature is high all the year round, the annual average temperature is above 22℃, and the most Leng Yue in winter is generally above 16℃ for half a year. In Xishuangbanna, Yunnan, and southern India, the alpine plateau in the north blocks the southward invasion of cold air, making the temperature in this area relatively high in winter and half a year, although the latitude is relatively high.

2. The dry and wet seasons are obvious, and the precipitation is concentrated in the rainy season, with a large amount of precipitation. 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 of the year, because the sun has begun to directly heat the northern hemisphere. 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.

The monsoon is extraordinary. In dry season, the northeast monsoon launched by land high pressure flows into the equatorial convergence zone on the ocean. In the rainy season, the southwest monsoon from the subtropical high in the southern hemisphere flows into the Tal low.

4. Tropical cyclones prevail. Synchronized with the "summer monsoon", tropical cyclones prevail from mid-May to mid-September every year.

The Indian Peninsula and Indo-China Peninsula are typical and major areas of this climate. However, the start and end times of the two seasons are different: the Indian Peninsula is usually rainy from June to September, and June to May is the dry season. In the late dry season (April-May), the weather is extremely hot, and the highest temperature is often above 40℃. The rainy season is full of rainfall, which often causes floods. Indochina Peninsula is usually rainy from May to 10, and dry from 1 1 to April of the following year. April or May is the hottest month, and the highest temperature is generally between 38-40℃. In rainy season, there are many convective rainfall and typhoon rainstorm, and lightning and thunder often occur, causing huge property losses. High temperature throughout the year, divided into dry season and rainy season.