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What are the distribution and characteristics of tropical climate types?

1, tropical rain forest climate

Distribution law: both sides of the equator, (about 10 degrees north and south latitude).

Cause of formation: it is controlled by equatorial low pressure belt all the year round, showing upward airflow.

Features: It is hot and rainy all year round.

2. Tropical grassland climate

Distribution law: tropical rain forest climate latitude 10-20 degrees.

Cause of formation: controlled alternately by equatorial low pressure area and trade wind area.

Features: high temperature all year round, obvious in dry and wet seasons, sultry and rainy when controlled by equatorial low pressure belt, dry and rainy when controlled by trade wind belt.

3. Tropical desert climate

Distribution law: generally near the tropic of cancer (20-30 degrees) inland or the west coast of the mainland.

Cause of formation: it is controlled by subtropical high pressure area and trade wind area all the year round.

Features: high temperature and little rain, perennial drought.

4. Tropical monsoon climate

Distribution: South Asia and Southeast Asia (east coast of the mainland 10-25 degrees).

Reasons: the huge thermal difference between land and sea and the seasonal movement of the position of pressure zone and wind zone.

Features: high temperature all year round, with dry season and rainy season.

Temperate climate:

Subtropical monsoon and humid climate. Summer is hot and rainy, and winter is mild and rainy. Distribution: 25 ~ 35 N east coast of mainland. Reason: Sea-land temperature difference. Plant type: subtropical evergreen broad-leaved forest.

Mediterranean climate. Summer is hot and dry, and winter is mild and rainy. The west coast of the continent is 30 north latitude to 40 south latitude. Cause of formation: the westerly belt and subtropical high are alternately controlled. Plant type: subtropical evergreen broad-leaved forest (grapes, olives, etc. ).

Temperate monsoon climate. Summer is hot and rainy, and winter is cold and dry. The east coast of the mainland is about 35 ~ 55 north latitude. Cause of formation: the difference of thermal properties between land and sea.

Temperate maritime climate. It is humid all year round, mild in winter and cool in summer. 40 ~ 60 latitude north and south, west coast of the mainland. Reason: It is controlled by the mid-latitude westerly wind all the year round.

Temperate continental climate. The temperature difference between winter and summer is large, and there is little precipitation throughout the year. The continent within 35 ~ 50 north latitude. Cause: Far from the sea, high latitude.