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Numerical Simulation of Seeding Liquid Carbon Dioxide to Increase Precipitation

机译:液态二氧化碳增加降水的数值模拟

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Using the improved three-dimensional cloud numerical seeding model, an experiment of aircraft seeding liquid carbon dioxide (LC) coolant to increase rain on September 13, 2002 in Yan’an region of Shaanxi Province was simulated and it was compared with seeding AgI ice nuclei. Results show that seeding cloud by LC and AgI in the appropriate part can induce notable change to cloud microphysical and dynamical parameters, accelerate updraft, produce earlier precipitation, change ground precipitation distribution and increase total precipitation on the ground. LC and AgI have different seeding effect though they are seeded according to the seeding rate that each usually use in the appropriate part in the cloud. On the basis of numerical simulation output data, the mechanism of seeding LC to increase rain was analyzed. Results show that after seeding LC in the cloud, rain water first grow through the process of mature ice particle (mainly graupel) thaw to rain (MLxr) when fall below 0°C level with the result of earlier appearance of precipitation particle, then further grow up by cloud-rain water collision and ground precipitation increased and precipitation period extent consequently.
机译:使用改进的三维云数值播种模型,模拟了2002年9月13日在陕西延安地区播种飞机液态二氧化碳冷却剂以增加降雨的实验,并将其与播种AgI冰核进行了比较。 。结果表明,在适当部位通过LC和AgI播种云可以引起云微物理和动力学参数的显着变化,加速上升气流,产生较早的降水,改变地面降水的分布并增加地面上的总降水。 LC和AgI具有不同的播种效果,尽管它们根据各自通常在云中适当部分使用的播种率进行播种。在数值模拟输出数据的基础上,分析了播种LC增加降雨的机理。结果表明,在将LC播种到云中之后,雨水首先通过成熟的冰粒(主要为graupel)融化,然后在低于0°C时融化为雨水(MLxr),这是沉淀粒子较早出现的结果,然后进一步因雨水冲撞而长大,地面降水增加,降水期延长。

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