Overview of the winter and summer monsoon in our country, our country is a typical monsoon climate,

Hehe, 8th grade geography. The standard answer is:

1.Origin: Winter monsoon: Siberia in Russia and the Mongolian Plateau in Mongolia.

Summer monsoon: Tropical ocean surface of the Pacific and Indian Oceans.

2.Wind direction: Winter monsoon: northerly (northeast or northwest).

Summer monsoon : southerly (southeast or southwest).

3.Nature: Winter Wind: Cold and dry.

Summer monsoon : warm and humid.

4.Scope of influence: Winter monsoon: the vast area of eastern China (except the Qinghai-Tibet Plateau, Yunnan-Guizhou Plateau, Hainan Island, Taiwan).

Southeast monsoon: a vast area in the eastern part of China; Southwest monsoon: southwest China, South China, the middle and lower reaches of the Yangtze River and the Yellow River.

5.Climatic impact: winter monsoon: cold and dry, resulting in a large temperature difference between north and south in China.

Summer monsoon : warm and humid, southeast coast, bringing precipitation to form the rainy season.

Origin: South Pacific and Northwest Pacific; Siberia in Russia and the Mongolian Plateau in Mongolia.

Wind direction: southeast and southwest monsoons; Northwest monsoon.

Properties: Warm and moist; Cold and dry.

Affected areas: Coastal areas; Desert.

Impact on climate: make the climate warm and wet; Make the climate cold and dry.

The summer monsoon originates in the South Pacific and Northwest Pacific, the southeast is dominated by the southeast monsoon, and the southwest is dominated by the southwest monsoon. The summer monsoon is hot and rainy, so that the precipitation in our country is mainly concentrated in summer, making the southern part of the Yangtze River and South China a land of fish and rice, while most of the regions at the same latitude are deserts.

The winter monsoon originates in Siberia in Russia and the Mongolian Plateau in Mongolia, and the winter monsoon affecting China is mainly dominated by the northwest monsoon, which is dry and cold, resulting in a colder and drier winter in China than in the same latitude.

Winter monsoon: Siberia, Mongolia, northwest and northeast, cold and dry, northern China, resulting in a large temperature difference between north and south in winter.

Summer monsoon: Pacific Indian Ocean, southeast and southwest, warm and humid, southeast coast, bringing precipitation to form the rainy season.

The formation of northeast winds in winter: the formation of high pressure centers in Mongolia and Siberia, the southerly airflow from the Ruzen high pressure is affected by the geostrophic deflection force in the process of southward movement, forming northeast winds and northwest winds in the north of China, and continuing to blow southward to form northeast winds. The shadow is in South Asia, Southeast Asia and parts of southern China.

Formation of the southwest monsoon in summer: In summer, the pressure belt wind belt moves northward, and the southeast trade winds in the southern hemisphere cross the equator and are deflected by the geostrophic deflection force, forming the southwest monsoon. It affects South Asia, Southeast Asia and parts of the southern part of China.

Southerly winds blowing from the sea to the land prevail in summer.

The summer monsoon comes from the Pacific Ocean in the southeast and the Indian Ocean in the southwest, and is warm and humid in nature, and under its influence, precipitation generally increases, and rain and heat are in the same season. Under the influence of the winter monsoon in the interior of Asia, which is cold and dry in nature, most parts of China generally have less precipitation and low temperatures in winter, and the north is more prominent.

China is affected by the alternation of winter and summer monsoons, and is the most typical of the monsoon and the most significant monsoon climate in the world. Compared with other regions of the world at the same latitude, China has low winter temperatures, high summer temperatures, large annual temperature ranges, and precipitation is concentrated in summer, which is characteristic of continental climate. Therefore, China's monsoon climate is more continental, also known as continental monsoon climate.

The main feature is that the precipitation changes significantly throughout the year with the rotation of the monsoon.

1. The summer monsoon is relatively small, and the rainfall is concentrated in the southern region, with drought in the north and flooding in the south.

2. When the summer monsoon is relatively strong, the rainfall area is concentrated in the north and the north, and there is a flood in the north and drought in the south.

Monsoon climate: 1. Mixed type of continental climate and oceanic climate.

2. In summer, it is affected by the warm and humid air flow from the ocean, which is hot, humid and rainy, and the climate is oceanic.

3. 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.

The summer monsoon affecting China includes the southeast monsoon from the Pacific Ocean and the southwest monsoon, southwest monsoon and southeast monsoon from the Indian Ocean.

2.The summer monsoon refers to the prevailing winds that blow from the ocean to the continent in the monsoon region in the summer. Due to the fact that the Asian continent is controlled by a huge thermal depression in summer, there is high pressure over the ocean, and the air flow blows from the high pressure area to the low pressure area.

The outbreak of the South China Sea summer monsoon marks the transition from winter circulation to summer circulation, and also indicates the arrival of the dry monsoon in East Asia and the beginning of the rainy season in China.

Its activity can have an important impact not only on the Asian monsoon system, but also on circulation and weather in the Northern Hemisphere. The outbreak date of the South China Sea summer monsoon has become one of the key contents of the annual "Flood Season Climate Trend Consultation" in South China, and with the development of economy and agriculture, the South China Sea summer monsoon has been more and more highly valued by all countries in the world, especially the countries and regions around the South China Sea.

The summer monsoon refers to the prevailing winds that blow from the ocean to the continent in the monsoon region in the summer. Due to the control of a huge thermal depression over the Asian continent in summer, there is high pressure over the ocean, and the air flow blows from the high pressure area to the low pressure area. The outbreak of the South China Sea summer monsoon marks the transition from winter circulation to summer circulation, and also indicates the arrival of the East Asian summer monsoon and the beginning of the rainy season in China.

Its activity will have a significant impact not only on the Asian monsoon system, but also on circulation and weather in the Northern Hemisphere. The date of the outbreak of the South China Sea summer monsoon has become one of the key contents of the "Flood Season Climate Trend Consultation" in South China every year, and with the development of economy and agriculture, the South China Sea summer monsoon is also more and more popular with countries around the world.

Chinese monsoon climate characteristics: The dry and wet seasons are obvious, and the four seasons are distinct. Winter is controlled by the northerly monsoon from high latitudes, and the climate is dry and cold, and the wind is strong.

In summer, the climate is mainly affected by the southerly air flow from the ocean, and the climate is hot and humid and rainy. The transition season is the interaction of these two types of control airflow, and the weather is changeable, such as cold, hot, sunny and rainy. The rainy season starts and ends with a clear regularity.

Early in the south, late in the north, early in the east, and late in the west. The rainy season ends, early in the north, late in the south, early in the east, and late in the west. Due to the influence of the monsoon, the eastern coastal area is more rainy, the western part is dry and less rainy, and the south is more rainy than the north.

Sooner or later, the occurrence of monsoon rains will have a profound impact on agricultural production, and may even cause large-scale floods and droughts. In northern China, the winter is dry and cold, and the summer is humid and hot, and the annual and diurnal variation of temperature is greater than that in southern China. There is a big difference in temperature and humidity between the north and south of China, and the difference in winter is greater than that in summer.

In winter, the temperature in eastern China is cooler than in the rest of the world at the same latitude.