After coming out of the prehistoric biological laboratory of K-3018, people also began to walk into the subject, and the people of the Land Administration and a large number of "national teams" came to the Matrix Science and Technology headquarters.

Half an hour later, Ren Hong arranged for everyone to come to a conference room to start discussing how to renovate the 330,000-square-kilometer Taklamakan Desert.

In the conference room, a group of scientists and the Land Administration and Kang Tao and others sat on the table, while Ren Hong was in front of the meeting, in front of a huge bright screen, the screen showed the topographic map of the western part of the country, and the Tarim Basin was in the middle of the screen.

“On the project to renovate the world's second largest mobile desert.”Ren Hong looked at everyone, he looked back at the screen and said, "I have to start from the climate, the Tarim Basin is a typical continental monsoon climate, drought!"

“If you want to change, you have to start with the root cause.The Taklamakan Desert Desert has accumulated sand during the Cretaceous period, and it has only evolved into the great desert of today.The typical reason is the topographical structure of the western part of China, the Tarim Basin is surrounded by mountains, the Tianshan Mountains in the north, the Pamir Plateau in the west, the most important thing is the super-high Himalayas and the Kunlun Mountains in the southern region, and the southeast is also the highest plateau in the world standing here, resulting in the Indian Ocean water vapor can hardly enter the Tarim Basin, the western Pamir Plateau blocking the humid ocean airflow, the southeast monsoon and southwest monsoon can not blow into the Tarim Basin.

Ren Hong pointed to the map and said: "This plateau and mountains also block the dry hot west wind in Central Asia to move north, which is undoubtedly the fire to add fuel, the dry west wind in Central Asia can not be dispersed here, the Tarim Basin is surrounded by thousands of meters of mountains and plateaus, many azimuth of wet water vapor is blocked from the outside, the most fatal is the Tarim Basin coordinates area is not in the monsoon area, Central Asia drought and raging west wind has been directly controlled."

A meteorologist sitting in the forefront also began to speak, he said: "On the issue of water vapour transmission in the southern region, over the years my team has carried out long-term field surveys, and after investigation and years of observation, we have come up with some results, we believe that the problem of water vapor sources in Taklamakan is basically caused by the evolution of the weather in the mainstream system of the outer circulation, rather than the inner cycle of the Tarim Basin, surrounded by the high mountain plateau, and the middle and lower water vapor transmission is very little, even almost zero."

"A series of studies have found that the vertical transportation of water vapor is relatively abundant.The area where the Tarim Basin is located reduces the vertical transport of the atmosphere in the lower and middle airspace horizontally, and when the convection clouds in the region move slowly in the summer, this convection effect greatly increases the amount of vertical water vapor transportation.Our study found that vertical convection in the Tarim Basin region is very strong, especially in summer, but unfortunately, vertical convection, although strong, vertical ascent is equally strong, while the ground layer in the Tarim Basin has a small humidity, which can reach almost zero index and the water vapor transmission volume is indirectly reduced.”

Listening to the silent nod, the meteorologist continued: "But it is worth mentioning that, on the contrary, the middle and lower levels of the region are very large, often under the influence of the external monsoon water vapor horizontal output, in the vertical convection effect, in theory, this will often produce a large number of heavy rain, as in July 23, 1988, the storm of heavy rain."

"As far as I know, that heavy rain was a special case."Ren Hong said, turning around to expand the map to the whole of Asia, he stared at the screen and said: "The large amount of precipitation generated in the eighties is due to the southward advance of the European high-pressure ridge, the northward trough from western Siberia to Central Asia blocked the eastward shift of the low vortex, and the subtropical low-wave trough in the southeastern region is caused by the subtropical low wave trough due to the division of the Iranian region, and there is a short-term wave trough affected by the large amount of precipitation before the low vortex invasion."

Ren Hong looked back at the meteorologist and at the others, saying: "The water vapor transportation in the Taklamakan region comes from the four directions of movement, west, south and north, mainly in the west and north, while the water vapor in the eastern and southern parts of the summer can enter the Taklamakan region, but in July of the eighties, although the precipitation was as high as 45 mm, it was just an unexpected accident."

“It is true that precipitation in the Taklamakan region is actually not in the minority, generally around 50 to 60 mm, but it is basically in the high mountain area, the most typical is the Kunlun mountain northern slope area is particularly significant, and the evaporation of the desert area is quite large, and the water that really drops to the ground quickly penetrates the soil and is evaporating.”He glanced back at the map and said, “Fundamentally, the climate problem of high convection vertical transport in the Taklamakan desert is fundamentally not helpful in changing the local desert climate.”

“What does Mr. President think about this?Or a solution?”The meteorologist asked.

Ren Hong said, silent for a moment, organized a word in his mind, and then said: "The Tarim Basin's tough straight problem is still surrounded by mountains, affected by the geographical characteristics of the high mountain plateau, the outer cycle of the climate can not have a direct climate impact on the interior of the Tarim Basin."

“The solution to the problem lies in itself.”Ren Hong said so, which makes the number of experts present curious.

“Many things, they will be able to solve their solutions, or weaknesses disguised as strong, and thus ignored.”Ren Hong said that this sentence is undoubtedly a lot of trouble for everyone, but there is no question, Ren Hong apparently did not finish, for a moment, he continued: "The core factor that causes the current climate in the Taklamakan region is the cause of geographical characteristics, and the answer to the problem is here."

“What do you say about that?”There is a very difference between the meteorologists sitting in the front row.

Ren Hong once again looked at the map in the concentrated screen and said: "Please look at the geographical characteristics of the Tarim Basin, surrounded by the high mountain plateau on all sides, the Tianshan in the north, the Pamir Plateau in the west, the Qinghai-Tibet Plateau in the southeast, the southern part of the Himalayas and Kunlun Mountains, the influence of the outer cycle climate can be ignored, and the four sides of the mountain caused the internal atmosphere to not go north, this series of factors can make the Tarim Basin have the climate characteristics of the inner cycle."

Ren Hong once again looked at all the human beings: "The solution to the problem is to form a relatively humid internal circulation climate in the lower and middle airspace of the Tarim Basin, independent of the external climate cycle, in short..."

“Our starting point is the issue of its inner circle!”