How to "make rainmakers"?
Hangzhou Shallow-Sea Technology Co., LTD.PubDate:2021-06-04 Hangzhou Shallow-Sea Technology Co., LTD. ViewNum:67

Artificial weather





What is weather modification

    Weather modification refers to the transformation of weather phenomena in a predetermined direction by artificial means under appropriate weather conditions. International weather modification began to rise in the 1950s, during which some famous scientific experiments were carried out, and the development of weather modification was promoted. Following the international pace, China has also carried out research on weather modification. After continuous off-site and indoor tests, a cloud-seeding and hail suppression system using aircraft, anti-aircraft guns and rockets as the main means has been preliminarily formed. At the beginning of the 21st century, due to the need of drought prevention, disaster reduction and improvement of the ecological environment, the scope of weather modification services has been expanded, has been extended to artificial rain reduction, fog reduction and forest fire prevention and other fields.


    During a forest fire in Yalong River town, Muli County, Liangshan Prefecture, Sichuan Province, in 2019, Samsung General Airlines, under the direction and coordination of the Sichuan Meteorological Bureau's Human Figure office, carried out aerial rain raising operations, which "created" 3.5 millimeters of rain in Liangshan area during the dry season, effectively reducing the spread of the fire. Taiwan Province is experiencing a drought this year, which is rare in decades. The effective water storage of major reservoirs in the southern part of the province was less than 20 percent in March. Can artificial rain be used to "create" precipitation to alleviate the drought? It should be noted that weather modification is not equal to artificial weather manufacturing, which needs to be carried out smoothly under specific conditions and achieve the desired effect. So what is the appropriate conditions for cloud-seeding?


Artificial rain enhancement operation

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What is weather modification



Conditions of rainfall

1、Natural rainfall

    Precipitation is the phenomenon that the water in the cloud falls to the ground in the form of liquid or solid state. The formation of precipitation needs three basic conditions: sufficient water vapor; The gas block can be lifted and cooled to condense; More condensation nuclei. The natural precipitation process is generally divided into two stages: cloud formation and precipitation. The cloud formation process is caused by the air block in the atmosphere being lifted and cooled, so that the water vapor in the air reaches the saturated or supersaturated state. The precipitation process is the growth of large and small cloud droplets into precipitation particles through the collision process and the transformation of ice water.


Schematic diagram of rainfall mechanism

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2、Artificial precipitation conditions and methods

  We cannot change the cloud formation stage of natural precipitation. We can only rely on nature to select objects that can produce precipitation for artificial influence. We can sow cold cloud catalyst (dry ice, artificial ice core) or warm cloud catalyst hypersonic core (such as salt particles) in the cloud body with potential to accelerate the condensation or consolidation of cloud droplets to form precipitation.


  Artificial precipitation methods include: ground layout AgI combustion furnace as the main means of ground precipitation (adapted to often have topographic cloud development, inconvenient transportation in mountainous areas), anti-aircraft artillery and rocket-based ground operations (adapted to work in the fixed target area, there are strong convective clouds under the case of catalytic operations), aircraft catalytic operations. Catalytic operation flexibility, can accurately grasp the plane position, and can use the plane in front of the catalytic homework imager loaded particle detector, such as precipitation, cloud combination detector, aerosol detector to detect in the air, such as the content of each particle concentration, get the cloud master appropriate catalytic place and time, to provide help for artificial precipitation enhancement operation, Reduce the blindness of cloud-seeding operation.


Airborne detection probe

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Conditions of rainfall



Aircraft detection test research

  Because of the different weather conditions and the structure of cloud, cloud around the micro physical characteristics are also different, the plane detection can be used to accurately to xiao yun, big cloud particles in a cloud, precipitation particle, particle concentration, effective diameter of aerosol particles and particle distribution, etc., thus the analysis of features of various physical quantities, it is the timing of the local precipitation enhancement. At present, many scholars have made certain analysis of the local cloud microphysical characteristics by using the experimental data of aircraft detection. The following is a brief list of the research and analysis of a detection result in Hebei, Guangxi and Sichuan.


   Hebei: The stratiform cloud precipitation system in spring in Hebei Province is uncertain, and there is a strong precipitation cloud band. It is concluded that the ice crystal scale in the cold cloud increases with the decrease of height, and the ice crystal grows fastest between 3400 m and 3100m, and the ice crystal particles are easy to cling and stick. The ice crystal concentration is the largest at 4400m, and the liquid-water content is the largest at 4000m. Since the ice crystal consumes supercold water, the supercold water content corresponding to the larger ice crystal concentration value is less.


    Guangxi: The analysis of the detection data shows that the stratified warm clouds are obviously stratified in the vertical direction. The non-precipitation clouds are generally single-layer or two-layer structures with large or small spacing, while the precipitation clouds are mostly composed of two or more layers with small spacing between layers, and temperature inversion occurs near the cloud tops. The cloud droplet concentration is the largest in the lower cloud base close to the ground, and the liquid water content and the effective diameter of the cloud droplet have the minimum values at the cloud base, which first increase and then decrease with the height, and generally there is a peak region in the middle of the cloud.


    Sichuan: The cloud system is a mixture of upper cold and lower warm, the warm layer is about 3200m thick, and the supercooled layer is 1800m thin. The top of the detection cloud system is the seeding layer, with more ice crystals, which are spread downward as condensation nuclei. The ice crystals increase rapidly in the supercooled layer and fall below the 0℃ layer, and the ice crystals melt into water droplets. At the same time, there are precipitation elements in the warm layer to initiate collision, and the warm cloud process can start.


Research on aircraft detection test



An introduction to aircraft detection

   The plane flew almost in a cold cloud, according to data from an aircraft survey conducted by Samsung General Aviation over the Sichuan Basin. The first cloud entry height is 4976m, and the lowest cloud entry height is 2363m. During the period, the layer cloud with 753m thickness passes through. The 0℃ altitude layer in the ascending stage is 3339m, and the 0℃ altitude layer in the descending stage is 2574m. In addition, most of the flight was in the seeding area, and a small part was in the strong seeding area. In the seeding area, there was a rich cloud water area. The average supercooled water content was about 0.2g/cm3, and the temperature was about -5℃. According to the CIP particle image, there was a seeding layer with rich ice crystal content in this flight, which provided certain help to judge the timing of artificial precipitation operation.


Cip particle image

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(Article source: wechat official account of Aviation Meteorological Innovation and Application Joint Laboratory)





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