卫星反演过冷层云中AgI播种轨迹的微观结构

D. Rosenfeld, Xing Yu, J. Dai
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引用次数: 22

摘要

美国国家海洋和大气管理局(NOAA)先进甚高分辨率辐射计(AVHRR)图像揭示了中国中部厚过冷层云中明显的冰川云轨迹。这些轨迹被认为是在- 10°C等温线上,在云顶以下不到1公里处,利用AgI丙酮发生器进行人工降雨作业而产生的,目的是增强降水。通过检索云顶有效半径(re),分析其与云顶温度和可见光反射率的空间关系,推导出云的组成。云顶温度在- 13°和- 17°C之间变化。在播种后约22分钟,云顶的冰川作用开始明显。冰川覆盖的顶部下沉并在过冷层云中形成通道。大约40 cm s−1的下沉速率与在这种条件下可能形成的冰晶的下落速度是相容的。在每小时38到63分钟之间,一条细细的新水云线在种子轨道的通道中央形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Satellite-Retrieved Microstructure of AgI Seeding Tracks in Supercooled Layer Clouds
Abstract NOAA Advanced Very High Resolution Radiometer (AVHRR) images revealed conspicuous tracks of glaciated cloud in thick supercooled layer clouds over central China. These tracks were identified as being artificially produced by cloud-seeding operations at the −10°C isotherm, less than 1 km below cloud tops, aimed at precipitation enhancement, by means of AgI acetone generators. The cloud composition was deduced by retrieving the cloud-top effective radius (re) and analyzing its spatial relations with cloud-top temperatures and with the visible reflectance. Cloud-top temperature varied between −13° and −17°C. The glaciation became apparent at cloud tops about 22 min after seeding. The glaciated tops sank and formed a channel in the supercooled layer cloud. The rate of sinking of about 40 cm s−1 is compatible with the fall velocity of ice crystals that are likely to form at these conditions. A thin line of new water clouds formed in the middle of the channel of the seeded track between 38 and 63 min a...
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