The dividing line between monsoon and non monsoon zones in our country is:

The dividing line between the monsoon and non-monsoon regions in China is roughly from northeast to southwest, from the Daxing'an Mountains - Yinshan - Helan Mountains - Bayankala Mountains - Gangdis Mountains

Therefore, the answer is: Daxing'an Mountains - Yin Mountain - Helan Mountain - Bayan Kala Mountain - Gangdis Mountain

The boundary between the monsoon climate zone and the non-monsoon climate zone is from the Daxing'an Mountains, the Yinshan Mountains, the Helan Mountains, the Wusheling Mountains, the Bayankala Mountains, the Tanggula Mountains, and the Gangdis Mountains. To the east of this boundary is the monsoon zone, in which the northerly winds prevail and the climate is dry and cold near the surface in winter, and the southerly winds prevail in the summer and the climate is humid due to the southerly winds controlled by the low-pressure system.

To the west of this dividing line is a non-monsoon zone with an arid climate.

The first line of Daxinganling - Yinshan - Helan Mountain - Bayan Kala Mountain - Gangdis Mountain. The vast area to the east and south of the line is the monsoon region of China; The area to the west and north of the line is the non-monsoon area of China.

The dividing line between monsoon and non-monsoon areas is the 400 mm isoprecipitation line.

That is, the Great Khing'an Mountains - Yin Mountain - Helan Mountain - Bayan Kala Mountain - Gangdis Mountain.

Xing'an Mountains, Yinshan Mountains, Helan Mountains, Wusheling Mountains, Bayan Kala Mountains, Tanggula Mountains, and Gangdis Mountains.

Monsoon and non-monsoon areas in our countryThe dividing lineIt is the 400mm isoprecipitation line, ieGreat Khing'an Mountains-Yin Mountain-Helan Mountain- Bayankala Mountain-Gangdis Mountain. Monsoon zones are areas where the climate is affected by the monsoon, while non-monsoon zones are areas that are not affected by the monsoon.

Monsoon refers to the wind that changes its direction regularly with the seasons. When many people study geography, they will find that the dividing line between monsoon and non-monsoon areas is often mentioned.

Our country has a monsoon climate.

A very obvious country, because of the size of our country and the fact that parts of our country will be affected by the monsoon. The monsoon climate will have a monsoon climate where the monsoon zone is located, and the monsoon climate will have a corresponding effect on the climate of the area, and the climate changes differently in summer and winter, because the climate changes with the monsoon. The monsoon climate zone in summer is characterized by very high temperatures and abundant rainfall, and the entire area is humid.

<>1. The boundary between the monsoon area and the non-monsoon cherry blossom area in China: Daxing'an Mountains-Yinshan-Helan Mountain-Bayankala Mountain-Gangdis Mountain, with the monsoon area in the east and the non-monsoon area in the west.

2. Causes of monsoon and non-monsoon regions: the difference in thermal properties between land and sea. The summer monsoon that affects China includes both the southeast monsoon from the Pacific Ocean and the southwest monsoon from the Indo-Tongdu Ocean.

Because the non-monsoon area is not affected by the summer monsoon shadow ridge, the northwest inland is not significantly affected by the monsoon, and the rainfall is less (the annual precipitation is less than 400mm), and the climate is arid.

The boundaries between the monsoon area and the non-monsoon area are the Daxing'an Mountains, Yinshan Mountain, Helan Mountain, Bayankala Mountain, and Gangdisi Mountain.

The northwest of the line is a non-monsoon area, and the southeast is a monsoon area.

In China, the area that is significantly affected by the summer monsoon is called the monsoon area, and other areas are called the non-monsoon area.

The summer monsoon that affects our country includes both the southeast monsoon from the Pacific Ocean and the southwest monsoon Lianglaohail from the Indian Ocean. Because the non-monsoon area is not affected by the summer monsoon, the northwest inland is not significantly affected by the monsoon, and the rainfall is less (the annual precipitation is less than 400mm), and the climate is arid.

The dividing line between monsoon and non-monsoon areas in China: Daxing'an Mountains - Yinshan - Helan Mountains - Bayanka Zhengtanla Mountains - Gangdis Mountains.

Monsoon, geometeorological concept. Because the continents and oceans heat up and cool differently throughout the year, a wide range of winds between the continents and the oceans that change direction regularly with the seasons is called a monsoon. The most fundamental reason for the formation of monsoon is the difference in the properties of the earth's surface and the difference in thermal response.

Caused by factors such as land and sea distribution, atmospheric circulation, and continental topography, the phenomenon of opposite wind directions prevails in a wide range of winter and summer seasons with a one-year cycle.

It is divided into summer monsoon and winter monsoon. The monsoon climate zone is generally affected by the ocean airflow in summer and the continental airflow in winter, and is mainly characterized by dry winter and wet summer. Our country is a typical monsoon climate zone.

There are at least six summer monsoon circulation systems in the world, including the Asian monsoon, the North African monsoon, the North American monsoon, the Australian monsoon, the South African monsoon and the South American monsoon, and each monsoon system can also be divided into several sub-monsoon regions.

Features of the monsoon.

The monsoon climate is characterized by hot, humid and rainy summers and cold, dry and rainy winters. The monsoon climate is the main feature of our country's climate, which is affected by warm and humid airflow in summer, and the high temperature and rainy period are basically the same, and the winter is affected by dry and cold airflow, and the climate is relatively cold.

The monsoon climate is affected by the warm and humid air flow from the ocean and the cold air flow from the continent, this climate is very favorable for the development of agriculture, the summer crop growth period, need a lot of water, this time is also a rainy period, so it is very beneficial to the growth of crops. From the perspective of precipitation areas, the annual precipitation in our country decreases from east to west.

East Asia, South Asia, and Southeast Asia are very typical monsoon climate zones, but the characteristics of the monsoon climate are different because of the geographical location. The formation of the East Asian monsoon is caused by the thermal differences of the sea routes and the seasonal movement of the planetary wind belt, while the South Asian monsoon region is generally characterized by a weak winter monsoon and a strong summer monsoon.

The dividing line between monsoon and non-monsoon areas is the 400 mm isoprecipitation line.

That is, the Great Khing'an Mountains - Yin Mountain - Helan Mountain - Bayan Kala Mountain - Gangdis Mountain.

The Great Wall --- the Great Wall of the Great Khing'an Mountains -- the Hengduan Mountains --- the eastern part of Qilian Mountain.

What is the Great Khing'an Mountains - Yin Mountain - Helan Mountains - down? Behind is Bayankala Mountain, Gangdis Mountain, Bayankala Mountain, Gangdis Mountain, and down is Bayankala Mountain.

The dividing line between the monsoon and non-monsoon regions in China is:

In the monsoon area east and south of the line of Daxing'an Mountains-Yinshan-Helan Mountain-Bayankala Mountain-Gangdis Mountain, precipitation is abundant, mainly concentrated in summer.

In the non-monsoon area, due to the influence of topography and other factors, the summer monsoon is difficult to reach, precipitation is scarce, and it is relatively dry throughout the year.