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China is located in the southeast of Eurasia, the world's largest continent, and borders the world's largest ocean, the Pacific Ocean.
The monsoon climate is particularly significant due to the thermal difference between land and sea, making China one of the most significant monsoon countries in the world. The winter monsoon comes from the hinterland of Asia at the middle and high latitudes, where temperatures drop sharply, creating a cold wave. The summer monsoon through the vast ocean brings abundant rain to Chinese mainland, so the rain in most parts of China is concentrated from May to September.
The morning and evening of the rainy season in various parts of China and whether it is normal or not are mostly directly related to the advance and retreat of the monsoon, and once the monsoon pattern is abnormal, there will be a wide range of drought and flood disasters. For example, in the summer of 1959, due to the strong warm and humid air of the southeast monsoon, its frontal heavy rain belt unusually moved northward, causing a drought in the middle and lower reaches of the Yangtze River, which usually has more plum rain in early summer, for two months, and a similar situation in 1978. In the summer of 1954, on the contrary, the southeast monsoon was blocked by cold air from the north, and until the end of July, the heavy rain belt was still stagnant in the Jianghuai River Basin, so that the middle and lower reaches of the Yangtze River basin experienced heavy water that had not been seen in a century.
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Backed by the largest continent and close to the largest ocean, the monsoon climate is remarkable.
In summer, China is generally hot and rainy, and in winter, the temperature difference between north and south is large, and the oceanic climate in coastal areas is obvious.
That's what the high school geography book says when it summarizes the characteristics of our country's climate.
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China's climate is characterized by the tropical monsoon region, the climate is very complex and diverse, the main characteristics are that the temperature difference between the north and the south is relatively large, the terrain and altitude are relatively high, and in the Qinghai-Tibet Plateau, especially in winter, the temperature gap between the north and the south is relatively large.
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The main climate characteristics of our country are that the climate is very complex and changeable, and the monsoon climate is very significant. The main characteristic is that the climate is changeable, and the monsoon climate is particularly obvious, as well as the temperate monsoon climate and the temperate continental climate, the terrain is high in the altitude area, and the plateau climate.
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China's climate characteristics are very obvious monsoon characteristics, the seasons are distinct, there is a regular seasonal change, generally high temperature and rain in summer, cold and dry in winter. The main feature is that the south is more humid and warm, and the north is drier and colder in winter.
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China's climate is characterized by the tropical monsoon region, the temperature difference between the north and the south is very large, the coldest in winter, the isotherm is roughly distributed along the Qinling Huai River, so the temperature difference is relatively large in winter, the average altitude of China's Qinghai-Tibet Plateau is more than 4 kilometers.
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The main characteristics of China's climate: the continental monsoon monsoon climate is significant.
The types of climate are complex and diverse.
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