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Landlord, your question has made you very stupid. The reasons are: 1. The Himalayas have been formed and are irreversible; 2. The Himalayas cannot be turned into plains; 3. Facts must be respected in scientific research; 4. In the face of nature, even if the talent is all over the world, it is useless to assume.
You might as well play with your hypothetical approach to climate research.
The terrestrial and sea-land structure indicates
The Himalayan mountain range region can never be turned into a plain.
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The result is more desertification than the current situation in India
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Of course, it is the warm and humid air flow north to North China! North China has become the climate type of the middle and lower reaches of the Yangtze River! The Tarim River flows into the Indian Ocean! Xinjiang's climate is also warming! The Tarim Basin has become a granary!! The disadvantage is that the source of the Yangtze River and the Yellow River has disappeared.
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You have to think about how to turn the Himalayas into plains, and then the rest, right?
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The whole of Asia has seen a sharp decline in life in three years! Sixty years later, everyone will be fine!
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The westerly wind prevails in the middle latitudes of the world, and the dynamic effect of the Qinghai-Tibet Plateau is that due to the existence of the Qinghai-Tibet Plateau, this westerly wind is divided into two branches, north and south, which continue to move eastward from the north and south of the plateau. In the Northern Hemisphere, northerly aircurrents bring more precipitation, while southerly aircurrents cause droughts. As a result, the southerpillar airflow will also carry a large amount of water vapor from the Indian Ocean on the northward airflow after bypassing the plateau, which will produce a large amount of precipitation in the middle and lower reaches of the Yangtze River.
In the 50s of the 20th century, Academician Ye Duzheng and Flohn respectively discovered that the Qinghai-Tibet Plateau is directly heated in the middle of the troposphere in a unique way in summer, becoming a powerful heat source for uplifting. In other words, thermal action refers to the Qinghai-Tibet Plateau due to its high terrain, which is a huge heat source in summer, resulting in a strong updraft, affecting the atmospheric circulation, and thus affecting the distribution of precipitation in China. On the contrary, winter is a huge source of cold, and the downdraft is strong.
Since most of China's water vapor ** is the Indian Ocean. Therefore, if the Qinghai-Tibet Plateau disappears, China's precipitation will decrease, which is what we are talking about, because of the existence of the Qinghai-Tibet Plateau, China's middle and lower reaches of the Yangtze River have become the only land of fish and rice in the same latitude in the world. However, in an academic report, Academician Wu Guoxiong also mentioned this issue, which also directly subverted my long-standing understanding of this issue.
He said that the thermal action of the Qinghai-Tibet Plateau causes a large amount of water vapor to be extracted from the lower latitudes. Without the Tibetan Plateau, water vapor would not have advanced to such a northerly place. However, this issue is still being debated.
For example, in 2010, Boos and Kuang, who are more famous in the domestic atmospheric circle, published an article in Nature that put forward different views, and Academician Wu Guoxiong published an article in SCI rep.Rebuttal made.
All of them involve experiments on the removal of the Tibetan Plateau using numerical simulations of the atmosphere. There are many other aspects. For example, many people on the mainland are doing snow cover in winter and spring on the Qinghai-Tibet Plateau, which affects the precipitation in East Asia by changing the perceived latent heat and surface albedo in the region and thus changing the atmospheric circulation.
However, these studies are still very preliminary, and there are still many problems. <>
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If the Himalayas suddenly turn into plains, the climate in northwest China and the Qinghai-Tibet Plateau will gradually warm and humid, and the landscape will gradually become southward, while the climate characteristics of India will decrease year by year, resulting in mild and rainy summers and colder and snowier winters. All in all, the change in the elevation of the Himalayas has both advantages and disadvantages for the Sino-Indian region, but in any case, the elevation of the Himalayas will not change much in a short period of time.
The high Himalayas block the warm and humid air currents from the Indian Ocean, making the climate in northwest China and the Tibetan Plateau dry and cold, and China's climate is becoming rich and diverse. Without the Himalayas, the warm and humid air currents from the Indian Ocean will continue to affect the atmospheric circulation in the Tibetan Plateau and the northwest region, making the local climate warmer and wetterNot only can it have a lot of perennial rivers and lakes, but it can also increase biodiversity, improve the climate and environment, and have many flora and fauna that can only be found in warm and humid regions.
Without the Himalayas, China would be a warm land without harsh climates, and many of its geographical boundaries would have to be redrawn, such as the equal precipitation lines. Among them, the area of humid areas will expand, the previously dry Gobi and land will be revitalized, forming speckled oases and water sources, and the desert will become a rare landscape, land and other related resources will have to be redivided, and many policies and decisions will be changed according to local conditions.
Without the Himalayas, cold air currents and cold waves from the Arctic Ocean would have swarmed up, adding to India's already cold winter, while warm and humid air currents from the Indian Ocean would not have climbed over the North Indian region to form terrain and would have lost some of India's precipitation. But the only benefit of the Himalayan subsidence for India is that it will alleviate the heat in the country, where the tropical climate will be mild.
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Then the temperature in India and China will become particularly high, and the wheels will be scorched every day when the car walks on the road. People can also suffer from heat stroke, and many industries will be shut down.
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If the Himalayas suddenly turn into plains, it will have a certain impact on the air in our country, and the air in our country may become even colder.
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We all know that the Himalayas are the world's largest mountains, and if they become plains, China's climate will become cold in all aspects, and the Himalayas are also a barrier against the cold climate.
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In the plateau and alpine regions of the middle and low latitudes, the climate varies vertically from the foothills to the summits, and there are different natural landscapes. The lower slopes of the high mountains are covered with trees, and the upper slopes are covered with young, low plants. At a certain height, the plants can no longer grow, and the top of the mountain is covered with snow and ice.
The climate on the top of the mountain is quite cold, and the plants cannot grow, only snow. In higher places, the climate is colder, and only plants that can adapt to cold climates can grow. The climate at the foot of the mountain is warm and there is a wide variety of plants.
Plateau climate refers to the climate that develops under the conditions of a plateau. The world's famous plateaus in the middle and low latitudes include the Qinghai-Tibet Plateau, Yunnan-Guizhou Plateau, Inner Mongolia Plateau and Loess Plateau in China, the Western Plateau of the United States, the Bolivian Plateau of South America and the East African Plateau. The climates are also different due to their geographical location, land and sea environment, altitude and plateau morphology.
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The monsoon climate is the main feature of the climate of our country. The monsoon climate is a mixture of continental and oceanic climates. 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, it is affected by the dry and cold air flow from the mainland, and the climate is cold, dry and rainy, and the climate is continental. In the monsoon climate, the summers are wet and rainy, and the winters are dry and rainy. The precipitation in China is mainly brought by the southeast monsoon, so the precipitation in China shows the characteristics of "decreasing from the southeast coast to the northwest inland" in geographical space.
If the Himalayas were in eastern Asia, then the monsoon climate would not exist! It will have a continental climate similar to that of Central Asia, which is arid and has little rainfall.
- - Foreign policy good ==
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