Why is the tropical monsoon latitude higher in India and lower in China?

Mainly affected by the topography, there are tall Himalayas in the north of India, and the terrain in the south is a low ancient plateau, which is lower and flat than in the north, and the warm and humid airflow from the ocean can go northward and easily form topographic rain when encountering the northern mountains, while there are no such topographic conditions in China's low latitudes, the terrain is relatively flat, and it is susceptible to the influence of cold air from the north, and the relatively high latitude position is not obvious by the warm and humid airflow from the ocean.

China has a large land area and many inland areas, the southern coastal area affected by the southwest monsoon is small, the central and southern parts of India are surrounded by the sea on three sides, and the western terrain is relatively low, which is conducive to the depth of marine water vapor.

Let's start by looking at what geographical borders. In addition, the temperature is greatly affected by topography and atmospheric circulation.

The latitude of China is high, so the temperature is lower. In addition, China is on the north side of the West Malaya Mountains, India is on the south side, and the warm and humid air flow of the Indian Ocean is blocked by the West Malaya Mountains and it is difficult to enter our country, so the temperature in China is lower than that of India. In addition, the temperature is greatly affected by topography and atmospheric circulation.

causes a difference in temperature.

The latitude of China is high, so the temperature is lower.

India is a tropical country.

China is a temperate country.

Plains account for about 40% of the total area, mountains only account for 25%, plateaus account for 1 3, but most of these mountains and plateaus do not exceed 1000 meters above sea level.

It is dominated by tropical monsoon climate, which is characterized by high temperature throughout the year, dry and rainy seasons. Northeast winds prevail in January, which is the dry season; Southwest winds prevail in July, which is the rainy season. At present, the most threatening meteorological disasters are floods and droughts, which are caused by the abnormal activity of the summer monsoon.

Flooding occurs when the wind is strong, comes early, and retreats late, and drought occurs when the wind is weak, comes late, and recedes early.

Coinciding with the "summer monsoon", tropical cyclone season is from mid-May to mid-September every year.

1.Because of latitude and longitude, the average temperature in India is hotter than in our country. 2.The topography of the east and west of our country is changeable.

3.There is a large temperature difference between the south and north of our country. The southernmost part is close to the equator, so the temperature will be relatively high, but the northernmost part is close to the North Pole, and some places are even covered with snow all day long, and the reason for this phenomenon is that the difference between north and south latitudes is too large, so their temperature difference is also very large.

This difference between the north and the south of our country also includes various topography reasons.

All in all, although India is relatively close to our country, there is still a big difference between the distance between the two countries and the equator, and many of India's land are closer to the equator than our country, so the average temperature is hotter. Whether it is east and west or north and south, the span is very large, there are plains, plateaus, and deserts, the southernmost weather is hot, and the northernmost is covered with ice and snow, which causes the temperature difference in our country to be relatively large.

India is hot all over the country, mostly in a tropical monsoon climate, while the Thar Desert in western India has a tropical desert climate. In summer, there is a more pronounced monsoon, while in winter there is no more pronounced monsoon. India's climate is divided into rainy season (June October), dry season (March May) and cool season (February of the following year), and in winter, it is affected by the Himalayan barrier, and there is no cold snap or cold high pressure southward affecting India.

India and South China are almost on the same latitude! But in the north of India, there is the roof of the world, the Himalayas, blocking the cold air from the south! So India is especially hot!

Suppose the Himalayas are moved to the location of the Qinling Mountains! Then the vast area south of the Yangtze River has become a tropical climate like India!

Can Sanya and Genhe be compared in China? Ten miles of different days, let alone thousands of miles. Don't ask this pediatric question anymore.

What's curious about this, because of the vast territory, the climate in a country is also very different, the south is full of spring flowers, the north is icy and snowy, the north is sowing, and the south is playing. The world is full of fragrant flowers in April, and the peach blossoms in the mountain temple are in full bloom.

Winters are also warmer in northern India, with large tropical areas. The eastern part of China is greatly affected by the winter monsoon, and the tropical area is small.

Russia is also close to China, why is there so much difference in temperature, one reason is that they are both territorial powers.

It's mainly because of the influence of different regions.

It's all the Himalayas that are to blame.

Because of the different temperature zones, India is mostly in the tropics.

Because the weather in India is different from China.

Because the two countries are not in the same temperature zone.

It is mainly affected by the air current.

It is the ignorant who ask this question.

It's like the territory of Russia, a country, but across the Eurasian continent! You tell me why!

In the Thar Desert on the northwest side of the Indian Peninsula, a typical tropical desert climate is formed. There are three reasons for this.

1) Related to low pressure in India:

The Thar Desert passes through the Tropic of Cancer and is located within the subtropical high pressure zone. In summer, a thermal low pressure is formed, but the upper altitude is still controlled by the subtropical high, and the downdraft prevails, forming a superposition of high and low pressure, so that the surface low-pressure airflow cannot rise further, and the convection is blocked, and it is not easy to form clouds and cause rain.

In spring and summer, it is the central part of India's lower Asia. However, due to the counterclockwise flow of cyclones in the Northern Hemisphere, the air flow in the Thar Desert region mostly comes from the Sahara and Arabian desert regions, and the water vapor is low and relatively dry.

2) Terrain-related:

The Indus Plain is located in the interior of South Asia and receives little precipitation due to the influence of the surrounding plateau mountains, especially the Iranian plateau. The end of the southwest monsoon from the Indian Ocean is already at the end of the strong crossbow, and the impact is weak; It is also blocked by the Iranian Plateau and the Suleiman Mountains, and it is difficult for water vapor to penetrate deeply. That is, the climate of the area of the leeward slope of the mountain.

3) Related to human activities:

There is a long history of human activity, the historical overexploitation of the Indus Valley, the destruction of ancient primeval forests, and the lack of vegetation protection on the ground. In addition, due to the deep groundwater burial in this area, the soil water content is less, the salt flats, cracked lands and other widely distributed, there is no plant growth in most areas, and a few plants that are resistant to dry and heat can survive, and the ecological environment is poor and fragile. According to scientists, the air over the Thar Desert is muddy, dusty, and gray during the day, and there are no stars at night.

On the one hand, dust reflects a part of the sunlight, and on the other hand, absorbs a part of the sunlight, causing it to warm itself and dissipate heat. Dust weakens solar radiation and prevents the ground from heating, thus creating an inversion layer that makes it difficult for the air to rise and thus become clouds and rain.

1 is related to the Indian low pressure: the Tropic of Cancer crosses and is located within the subtropical high pressure belt. In summer, a thermal low pressure is formed, but the upper altitude is still controlled by the subtropical high, and the downdraft prevails, which is dry and rainless, and it is not easy to form clouds and cause rain.

2.Topography-related: The Indus Plain is located in the interior of South Asia and is influenced by the surrounding plateau mountains, especially the Iranian plateau, with little precipitation. It is also blocked by the Iranian Plateau and the Suleiman Mountains, and it is difficult for water vapor to penetrate deeply. That is, the climate of the area of the leeward slope of the mountain.

3.The historical overexploitation of the Indus Valley, the destruction of ancient primeval forests, and the lack of vegetation protection on the ground. In addition, due to the deep groundwater burial in this area, the soil water content is less, the salt flats and cracked lands are widely distributed, and there is no plant growth in most areas, and the ecological environment is poor and fragile.

Please adopt!

Idea analysis: the northwest of South Asia - the latitude of the Indus River Basin, in winter by the subtropical high pressure, the air flow sinks, precipitation is scarce, in summer here is controlled by the low pressure in northern India, is the updraft, generally said that the updraft provides conditions for precipitation, but there is still little rainfall, the climate is relatively dry, this is because from the South Asian topographic map can be seen, the ground here is a desert, water vapor is less; Even in summer, the southwest monsoon blows, because part of it comes from the dry African continent; Although the other part reaches here through the Arabian Sea, because the Arabian Sea is only a few hundred kilometers wide, the water vapor that can be ** is also limited, although there can be some precipitation, but because the ground evaporation (about 3000 mm) greatly exceeds the precipitation (about 200 mm - 500 mm), so the tropical desert climate is formed.

The result of alternating control of the subtropical high and offshore trade wind belts.

When the subtropical high is controlled, the downdraft prevails, and the water vapor does not rise easily to cause clouds and rain, and when the offshore trade wind belt is controlled, the water vapor comes from the inland, so it becomes a desert climate.

Summary. India is located in the northern hemisphere, between 6°44' and 35°30' north latitude and 68°7' and 97°25' east longitude. India is the seventh largest country in the world, with a total area of about 3.17 million square kilometers.

With a total length of 3,214 kilometers from north to south and 2,993 kilometers from east to west, the Indian peninsula is also the main body of South Asia.

India is located in the northern hemisphere, between 6°44' and 35°30' north latitude and 68°7' and 97°25' east longitude. Yintan Bank is the seventh largest country in the world, with a total area of about 3.17 million square kilometers. With a total length of 3,214 kilometers from north to south and 2,993 kilometers from east to west, the Indian Peninsula is also the main body of South Asia.

India has a tropical monsoon climate in the south and a temperate climate in the north. Sudden floods caused by rain caused by dry drought and monsoon windy climate, severe thunderstorms, etc. are the major natural disasters in India. Read more**This article tests the university you can go to in Yunnan.

Southeast Asia is made up of Indochina Peninsula and the Malay Archipelago. Located in the Eastern Hemisphere, spanning the northern and southern hemispheres. From the perspective of the location of latitude and auspiciousness, most of Southeast Asia is located between the remaining 10°s and the Tropic of Cancer, which belongs to the tropics and is a low-latitude region.

The main climate type in India is tropical monsoon; It is characterized by high temperatures throughout the year, with obvious rain and drought seasons.

India has high temperatures all year round, with an average annual temperature of more than 22, and the coldest month is generally above 16. Usually from June to September, it is the rainy season under the influence of the southwest monsoon from the Indian Ocean. From October to May of the following year, it is the dry season due to the influence of the northeast monsoon from the Eurasian continent.