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The eastern part of the country has a monsoon climate.
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The eastern part of the country is a monsoon climate zone. Monsoon climate refers to the climate of the area dominated by the monsoon, which is continental and oceanic.
Hybrid type. In summer, under the influence of warm and humid air currents from the ocean, the climate is hot, humid and rainy, and the climate is oceanic. In winter, affected by the dry and cold air flow from the mainland, the climate is cold, dry and rainless, and the climate is continental.
Monsoon climate: As for the cause of the monsoon, it is believed that it is caused by the difference in heat between land and sea and the seasonal variation of this difference. It is believed to be caused by seasonal shifts in the planetary wind belt. Some climatologists in China believe that the monsoon phenomenon is the thermal effect and atmospheric circulation of the distribution of sea and land.
It is a comprehensive phenomenon under the combined influence of three factors, such as seasonal changes and specific topography. China has a vast territory, spanning the tropics, subtropics, and mid-latitude temperate zones from south to north. Northwest China Territories.
It is an inland area with a continental climate; In the east and south of China, it is the confluence area of the East Asian continent and the western Pacific Ocean, and the difference between sea and land heat is obvious, which is a typical monsoon climate zone. From south to north, it has a tropical and subtropical monsoon climate.
Temperate monsoon climate.
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Continental monsoon climate.
It is characterized by high temperature and rain in summer, and cold and dry in winter. Compared with the oceanic monsoon climate, the annual temperature range is large, the rainy season is short, and the annual precipitation is low. For example, Beijing, China.
<> contrast, the oceanic monsoon climate is characterized by warm and humid summers and low temperatures and little rain in winters. Compared with the continental monsoon climate, the summer temperature is slightly lower, the winter temperature is slightly higher, the annual temperature range is smaller, the annual precipitation is more, and the rainy season is longer.
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Summary. China is located in the southeast of the Eurasian continent, the largest continent on the earth, and is bordered by the largest ocean on the earth - the Pacific Ocean Due to the huge difference in the nature of the sea and land, the northern part of the Asian continent has become a gathering place of cold air in winter, with high air pressure, and cold air radiates from the center of high pressure to the surrounding areas; In summer, the land warms up rapidly and the air pressure is low, while the ocean pressure is relatively high, and warm and moist air blows from the ocean to the continent.
The eastern region is distributed with the most typical climate in the world + its outstanding characteristics are.
Hello, I am inquiring for you here, please wait a while, I will reply to you right away The eastern region has the most typical monsoon climate in the world.
China is located in the southeast of the Eurasian continent, the largest continent on the earth, and is bordered by the Pacific Ocean, the largest ocean on the earth. In summer, the land warms up rapidly and the air pressure is low, while the ocean pressure is clear or high, and warm and moist air blows from the ocean to the continent.
The monsoon climate has a great impact on China's economic development In the early days of the general high temperature in summer, the rain and heat are the same as the panicle, and the water and heat strips are properly coordinated, so that crops and trees can get sufficient heat and water during the vigorous growth period
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Summer temperatures in eastern China:
Eastern region in summer. In summer, the temperature difference between the north and south in the eastern part of China is much smaller in spring than in winter. The average summer temperature in most parts of Northeast China and North China is 16 24°C, of which the Greater and Lesser Khing'an Mountains, Changbai Mountains and the northern part of North China Doushen are below 20°C. The average summer temperature in most areas of the North China Plain and south of the first line of the Qinling Mountains and the Huaihe River is 24 28°C. Yunpao pins the rock-Guizhou plateau at 20-24 °C; The coastal and southern areas of Guangdong and Guangxi provinces are above 28°C.
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The climatic characteristics of the eastern part of China are: the monsoon climate is significantSummers are hot and rainy, and winters are cold and dry.
Rain and heat at the same time. The annual precipitation is about 1,000 mm, and about two-thirds of it is concentrated in summer. There are four distinct seasons throughout the year, and the weather can be changeable.
With the increase of latitude, the temperature variation in winter and summer increases correspondingly, while the precipitation decreases gradually.
Due to the influence of the monsoon, the temperature in the eastern part of the country varies greatly from year to year, and the temperature in winter is lower and the temperature in summer is higher than that of other parts of the world at the same latitude.
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