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Comparison Between Computer Simulation of Transport and Diffusion of Cloud Seeding Material Within Stratiform Cloud and the NOAA-14 Satellite Cloud Track

机译:层状云内云种物质的运移与扩散与NOAA-14卫星云轨道的计算机模拟比较

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摘要

A precipitation enhancement operation using an aircraft was conducted from 1415 to 1549 LST 14 March 2000 in Shaanxi Province. The NOAA-14 satellite data received at 1535 LST soon after the cloud seeding shows that a vivid cloud track appears on the satellite image. The length, average width and maximum width of the cloud track are 301 km, 8.3 and 11 km, respectively. Using a three-dimensional numerical model of transport and diffusion of seeding material within stratiform clouds, the spatial concentration distribution characteristics of seeding material at different times, especially at the satellite receiving time,are simulated. The model results at the satellite receiving time are compared with the features of the cloud track. The transported position of the cloud seeding material coincides with the position of the track. The width, shape and extent of diffusion of the cloud seeding material are similar to that of the cloud track.The spatial variation of width is consistent with that of the track. The simulated length of each segment of the seeding line accords with the length of every segment of the track. Each segment of the cloud track corresponds to the transport and diffusion of each segment of the seeding line. These results suggest that the cloud track is the direct physical reflection of cloud seeding at the cloud top. The comparison demonstrates that the numerical model of transport and diffusion can simulate the main characteristics of transport and diffusion of seeding material, and the simulated results are sound and trustworthy. The area, volume, width, depth, and lateral diffusive rate corresponding to concentrations 1, 4, and 10 L-1are simulated in order to understand the variations of influencing range.
机译:2000年3月14日LST 1415年至1549 LST在陕西省进行了一次飞机的增雨作业。云播种后不久,在1535 LST接收到的NOAA-14卫星数据表明,卫星图像上出现了生动的云迹。云径的长度,平均宽度和最大宽度分别为301 km,8.3 km和11 km。利用层状云中种子物质传输和扩散的三维数值模型,模拟了种子物质在不同时间,特别是在卫星接收时间的空间浓度分布特征。将卫星接收时的模型结果与云轨道的特征进行比较。播云材料的运输位置与轨道的位置重合。云播材料的宽度,形状和扩散程度与云道相似,宽度的空间变化与轨道的变化一致。播种线各段的模拟长度与轨道各段的长度一致。云迹的每个部分对应于播种线的每个部分的传输和扩散。这些结果表明,云径是云顶部云播种的直接物理反映。比较表明,运移与扩散的数值模型可以模拟种子材料运移与扩散的主要特征,模拟结果合理可靠。为了理解影响范围的变化,模拟了与浓度1、4和​​10 L-1相对应的面积,体积,宽度,深度和横向扩散率。

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