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Annual precipitation is very small, less than 200 mm of annual precipitation; Precipitation is unevenly distributed seasonally, with slightly more precipitation in some months and even no precipitation in some months.
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The tropical desert climate is extremely arid and extremely hot, with an average annual rainfall of less than 50 mm in most areas, and even no rain in some places for many years, making it the driest type of climate on earth. The scorching heat is a masterpiece of the desert, with absolute highs of over 50 and even higher ground temperatures.
The climate of tropical desert is characterized by high annual average temperature, large annual temperature difference, greater daily temperature difference, scarce precipitation, and annual precipitation of less than 125 mm. This climatic zone is widely distributed in the desert and has few organisms, with only sporadic drought-tolerant plants such as cacti. At the edge of the desert there is a sparse bush.
The vegetation type is tropical desert.
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There are five types of precipitation: year-round rainy type, year-round little rain type, summer rain type, winter rain type, and perennial humid type.
The type of precipitation in tropical desert climate is characterized by year-round low rainfall.
The picture above is the winter rain type.
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The causes of tropical desert climate are:1It is controlled by the subtropical high pressure belt.
2.Controlled by the drying trade winds. 3.
Affected by a cold snap. The subtropical high is a dynamic high pressure, which is formed by the continuous flow of air over the equator to the subtropical air and accumulation, resulting in a downdraft, resulting in an increase in low air pressure.
Tropical desert climates are found in the interior of the continent or on the west coast of the continent between the Tropic of Cancer and 30°N-south latitude, and extend inland, such as the desert areas of northern Africa, the Arabian Peninsula in Asia, and Australia.
The tropical desert climate is characterized by many sunny days, strong sunlight, dryness, hot summer, large temperature difference between day and night, and many winds and sands.
The Sahara Sand Hall Disturbance Desert in Africa, the Kalahari Desert, the Arabian Desert in Southwest Asia, the Thar Desert, the Western and Central Australia Desert, the California Desert, and the Atacama Desert in South America all have tropical desert climates of the classic Lieson type.
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The causes of tropical desert climate are:1It is controlled by the subtropical high pressure belt.
2.Controlled by the drying trade winds. 3.
Affected by a cold snap. The subtropical high is a dynamic high pressure, which is formed by the continuous flow of air over the equator to the subtropical air and accumulation, resulting in a downward airflow of Lu leakage, resulting in an increase in low air pressure.
Tropical desert climates are found in the interior of the continent or on the west coast of the continent between the Tropic of Cancer and 30°N-south latitude, and extend inland areas, such as northern Africa, the Arabian Peninsula in Asia, and the desert area of Australia.
The tropical desert climate is characterized by many sunny days, strong sunshine, dryness, hot summers, large temperature differences between day and night, and many winds and sands.
The Sahara Desert and Kalahari Desert in Africa, the Arabian Desert in Southwest Asia, the Thar Desert, the Western and Central Australian Desert, the California Desert, and the Atacama Desert in South America all have typical tropical desert climates.
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( Tropical rainforest climate ) Savannah climate ).
Tropical desert climate ).
Mediterranean climate ) temperate oceanic climate ) cold climate or polar tundra climate or polar climate ) ).
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Tropical monsoon climate characteristics: high temperature all year round, large annual precipitation, obvious dry season and rainy season.
Tropical desert climate characteristics: high temperature and drought all year round, annual precipitation is less than 500 mm, and even in many places the annual precipitation is less than 200 mm.
Temperate monsoon climate characteristics: hot and rainy in summer, cold and dry in winter. The average winter temperature is below 0 degrees Celsius, and the annual precipitation is less than 800 mm.
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