The Tarim River overflows in the Taklamakan Desert, forming numerous lakes , has the Loulan Oasis r

The Loulan Oasis can be realized, because another desert not far from the Taklamakan Desert has become an oasis, and it is easy to do it when there is water.

I think it is possible, and it also shows that our measures are doing relatively well, and there must be no problem in moving in this direction.

It probably won't happen again, because it's still very dry, and although there is a small amount of precipitation, it will soon evaporate, and the probability of an oasis is not high.

The Tarim River overflows in the Taklamakan Desert, forming numerous lakes, which are also a recreation of the Loulan Oasis, where the local climate changes.

Everyone wants to know how the lakes in the desert appeared, and every drop of water in the desert is very precious. Through the analysis and research of relevant personnel, we can know that the appearance of desert amber is a real thing, and such a beautiful scenery has also been photographed by everyone. This scenic spot has always been short of water, and now there are some lakes, mainly some poplar forests in the Tarim River Basin, some lakes formed by the decentralization of ecological water, and part of the Tarim River in September There is a warning flood situation, these waters are overflowing, and small reservoirs have appeared in some floodplains.

These small amber are formed in the desert and large areas of the desert are also covered by floods, so such a landscape is formed, mainly because there are heavy rains or natural leaks and some ecology in the local area, and the water becomes stagnant water, when these stagnant water has not penetrated into the desert, you will form in some low-lying places, and it looks like amber, although it will disappear, but it can also bring some relief to the local ecology. It makes people feel that the air is more humid and not particularly dry than the previous environment.

People believe that this is a reappearance of the Loulan Oasis, and in recent years, the warm and humid appearance in these places in the northwest of southern Xinjiang is particularly obvious, and there are some ** who will use such hot spots to hype. Many people also expressed doubts, because the current trend of climate warming is undoubted, and the precipitation in southern Xinjiang has also increased, and the precipitation itself is relatively small, and the increase is limited, which cannot meet the demand for evaporation. The local meteorological drought is very severe, through the relevant detection, the humidity here will also drop, and the air and water pollution will decrease, and the precipitation will also have extreme changes, which will affect the moisture in the soil, and the natural vegetation may also be degraded, so the overall climate will change.

XinjiangTaklamakan DesertThere are many lakes that are influenced by the following factors.

As the human factor continues to increase, the rate of global temperature increase is also accelerating, and this summer has seen rare sustained high temperatures in many places.

Take the Taklamakan Desert as an example, due to the subtropical high in the northwest Pacific Ocean.

Continued on the Tibetan Plateau.

The effects were sustained, while also bringing warm, moist air across the Tibetan Plateau and further north, encountering equally active cold air near the Taklamakan Desert.

The result is a very intense, very concentrated, but not long-lasting heavy rainstorm.

Also, due to the warming climate.

The summer wind and rain belt in East Asia moved northwards to North China and Northwest China.

The precipitation was also higher than in the same period of the previous year, which also led to the Tarim River in Xinjiang.

There was the most rain in a decade.

Due to glacial meltwater, 25 rivers in the main trunk and tributaries of the Tarim River have floods that exceed the warning water level, and their flood duration is long, the volume of water is large, and the number of floods is many.

Various branches of the Tarim River flooded early at the end of May; The runoff from the upper reaches of the Tarim River from the end of May to the end of September was more than double that of the same period of the year. The main stream of the Tarim River, heavy rain and floods.

Snowmelt floods and glacial outburst floods have appeared successively and have been superimposed many times.

These lakes in the Taklamakan region were caused by flooding from the Tarim River.

In dry, hot climates, most of the lake's water evaporates and is then blown away by the wind to other areas. In addition, some of the water seeps into the lower part of the desert and may connect with the groundwater at the bottom of the desert, where the oases can survive for a long time because of the recharge of groundwater.

In addition to the above two cases, the excess water will accumulate along the desert topography in the low-lying areas, forming a part of the lakes that dot the desert, and finally evaporate.

These lakes are due to the melting of glaciers due to high summer temperatures, and recent rainfalls.

I think it's due to the movement of the earth's crust, which causes the underground river to rise up in this area, thus forming a lake.

That must have been influenced by our society and human beings, mainly because they kept littering and didn't clean up.

These "desert lakes" are actually stagnant water formed by local torrential rains and floods on the Taklamakan Desert.

This is because the weather is abnormal, so the local rainfall has increased, and many lakes have formed.

The reason for the formation of the lake is that there is a lot of water in the Taklamakan Desert due to heavy rains in the area.

This year, the global warming effect has been particularly severe, causing the snow-capped mountains around the Taklamakan Desert to melt, which is why so many lakes have appeared.

Influenced by climate and topography, the Taklamakan Desert is located in the center of the Tarim Basin, with annual rainfall of no more than 100 mm and an average evaporation of 2,500-3,400 mm. Due to the continuous melting of glaciers due to global warming, the Tarim River basin has been experiencing warning floods since September. Small shallow shoals have formed in many places.

It was also a very hot year, with high summer temperatures accelerating the melting of glaciers, and the area received much more rain than usual due to the high temperatures.

Most of the northern tributaries of the Tarim River come from the Tianshan Mountains, and the southern tributaries come from the Kunlun Mountains, and the frequent outbreaks of floods have led to the emergence of small lakes in the Taklamakan Desert, although such a scene is not common, but the lakes in the Taklamakan Desert are only temporary, and will evaporate directly in the end, so the possibility of an oasis is not high.

The existence of desert lakes is actually relatively common, after these floods flow to the Taklamakan Desert, they will accumulate water on the surface of the desert to form a relatively wide area of water, and the underground layer of the desert itself will not have any effect, plus the drought of the desert itself, so these lakes will slowly evaporate. As the driest desert in the Taklamakan Desert, there are almost no animals and plants in the desert, and even if it is human, it is difficult to survive in a state of lack of water.

For Xinjiang locals, flooding and snow cover in the Tarim River in the Taklamakan Desert are common, after all, too much water in the Tarim River will end up in the Taklamakan Desert. There will also be strong winds and sandstorms in the desert, and it is difficult for this lake in the Taklamakan Desert to have an oasis, after all, what plants need is water, and if there is no water, they will basically not survive, which is why there are no animals and plants in the Taklamakan Desert.

The Taklamakan Desert in Xinjiang has formed many rich places, mainly because the Tarim River has abundant water this year. This also has a lot to do with the environmental protection work in recent years.

That's definitely where we intervene, because we protect the environment every day and plant a lot of trees.

This year is the largest year in the Tarim River in Xinjiang in the past ten years, and the river overflows into the nearby Taklamakan Desert, and many lakes have also appeared in the desert, the combination of desert and lake, the scenery is extremely spectacular, and many netizens are curious about why the Taklamakan Desert can't be planted with trees, see below for details.

When it comes to deserts, most people have the impression of a lack of water, dryness, heat, and no rain.

But recently, in the Taklamakan Desert in Xinjiang, sand dunes and lakes are intertwined in the same frame, and this peculiar scenery has made many netizens call it spectacular.

The cascading feeling of the desert and the blue water of the lake seem to give the desert a sense of flexibility. Under the influence of the lake's water, the sand dunes of the world are firmly adhered to each other, and the beauty is clear and intoxicating.

The Taklamakan Desert is located in the center of the Tarim Basin in southern Xinjiang, with a length of more than 1,000 kilometers from east to west and a width of about 400 kilometers from north to south, with a total area of more than 330,000 square kilometers, making it the largest desert in China.

The Taklamakan Desert is the second largest mobile desert in the world after the Sahara Desert in Africa, meaning "the place where you can't get in and out".

It is understood that this year is the largest year in the Tarim River in the past 10 years, and the river overflows into the nearby Taklamakan Desert, forming numerous lakes.

According to experts in the management of the desert, planting trees in the Taklamakan Desert will not improve its ecological environment, but will exacerbate the ecological crisis of the desert.

Planting trees here will allow the trees to absorb the small amount of water in the soil into the trunk, and then disperse it into the atmosphere through the transpiration of the leaves, eventually leading to the death of the trees and the lower water content of the desert, forming a vicious circle of more serious desertification.

Therefore, for the Taklamakan Desert, a desert formed by natural causes, we cannot simply use afforestation to control the model, if the wrong management method is used, it will exacerbate the degree of local desertification.

The best way to manage the sand dunes is to block the advance of the sand dunes and hold on to the good land. By building shelterbelts and windbreaks around the Taklamakan Desert, the speed of sand dunes can be reduced to minimize the impact of desertification on production and life, and the impact of windbreaks on cities can be reduced.

The Taklamakan Desert is the largest desert in China and is located in the southern Xinjiang region. It was originally an arid area, but in recent years numerous lakes have emerged in some areas. The appearance of these lakes is mainly influenced by the following factors:

1.Climate change: Global climate change has led to an increase in extreme weather events and an increase in precipitation. Climate change has led to an increase in rainfall in parts of the Taklamakan Desert, which is a key factor in the formation of the lake.

2.Seasonal rainfall: To some extent, precipitation in the Taklamakan Desert is mainly concentrated in the summer months. This rainfall accumulates in the desert and helps in the formation of lakes.

3.Groundwater recharge: The Taklamakan Desert is rich in groundwater resources. As rainfall increases, the recharge of groundwater increases, and lakes are formed.

4.River diversion: Some rivers may be diverted as they pass through the Taklamakan Desert due to changes in topography, depletion of water sources, etc. These diverted rivers may carry abundant bodies of water that provide the conditions for the formation of lakes.

5.Desert Vegetation Restoration: Over the past few decades, China** has taken a series of measures to improve the ecology of the Taklamakan Desert.

These measures include planting shelterbelts and sealing sand for grass cultivation. The restoration of these vegetation covers the Taklamakan Desert to improve the water status of the Taklamakan Desert, increase the utilization of precipitation, and promote the formation of lakes.

It is important to note that although some lakes have appeared in the Taklamakan Desert in recent years, the amount of water in these lakes is not enough to completely change the drought conditions in this region. Ecological restoration of the Taklamakan Desert remains a long-term and arduous task.

The formation of Taklamakan desert lakes is influenced by the following factors:

Water source: Water from precipitation, snowmelt or water systems is a prerequisite for the formation of lakes. The mountains surrounding the Taklamakan Desert may have provided water to the lake.

Sediment: The influence of desert topography slows down the flow of water, allowing sediment to settle down to form lakes.

Climate change: Climate change can lead to increases and decreases in precipitation, which in turn affects the formation and disappearance of lakes.

1. Climatic factors: The Taklamakan Desert is located in the inland region of the Central Asian continent, with an arid climate and low annual precipitation. However, due to the influence of topography and landforms, the desert surface is not flat, and there are some low-lying terrains that may form temporary lakes during the precipitation season.

2. Topographic and geomorphological factors: The Taklamakan Desert area is low-lying and has some basins and depressions. During the rain or snowmelt season, precipitation or snowmelt flows into these low-lying terrains, creating temporary lakes. These lakes may dry up or evaporate during the dry season.

3. Water supply: There are some mountains and rivers near the Taklamakan Desert area, which provide a part of the water supply. When there is too much precipitation or when rivers are at the same level**, water may flow through groundwater or surface water into low-lying terrain to form lakes.

4. Human activities: Human activities may also have an impact on the formation of lakes in the Taklamakan Desert. For example, activities such as artificial water diversion, irrigation of farmland, and industrial water use can lead to an increase in water sources, which in turn can lead to the formation of lakes.