移动湍流的波散射和风速测量

Yu.P. Akulinichev, A.M. Golikov, G.S. Sharygin
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引用次数: 0

摘要

由于对具有联合分集的对流层散射系统的分析取得了新的进展,用VHF/UHF双基地雷达测量低层大气中的水平风的问题得到了重新考虑。给出了小天线空间分集和大天线角分集的测量方法。对于交叉路径平均风速和大尺度空气涡度的联合测量,还需要估计沿路径的散射体积大小。在495公里海上跨地平线路径上的雷达风速估计与在4公里高度范围内的无线电探空数据进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wave scattering from moving turbulence and wind velocity measurements

The problem of measuring horizontal winds in the lower atmosphere with a VHF/UHF bistatic radar is reconsidered because of recent progress in the analysis of troposcatter systems with joint diversity. The measurement procedures for spatial diversity of small antennas and angular diversity of large antennas are substantiated. It has been established that for the joint measurements of crosspath mean wind velocity and large-scale air vorticity the size of the scattering volume along the path also has to be estimated. Radar wind velocity estimates over a 495 km sea trans-horizon path are compared with radiosonde data over the height range up to 4 km.

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