面积测风法  

Computational method of anemography by proportion

作　　者：王烨芳[1] 齐久成[1] 马朝军[2] 王威[1] 

机构地区：[1]中国白城兵器试验中心 [2]75810部队90分队

出　　处：《气象水文海洋仪器》2009年第1期12-16,共5页Meteorological,Hydrological and Marine Instruments

摘　　要：文章通过对单经纬仪测风法和基线测风法的分析研究,总结了其各自的优点和不足,并根据需要在吸收基线法测风优点的基础上,提出了一种基于基线法测风的新型测风方法——面积测风法。介绍了面积测风法的计算方法,并重点阐述了其与基线测风法的对比分析以及在风廓线雷达等定型试验和轻兵器试验中所起的重要作用,结果表明面积测风法具有很高的实用价值。This article summarizes the advantages and disadvantages of single theodolite wind measurement and base line through the analysis of single theodolite wind measurement and base line wind measurement. On the base of absorbing the advantages of base line wind measurerment, this article put forwards a new method of wind measurements-area wind measurement which base on the base line wind measurement, according to the actual requirement. After introducing it, this article lays heavy stress on the comparative analysis of area wind measurement and base line wind measurement along with its important role in the type tests of windprofilers and so on,as well as in small arms and low ballistic ordnance tests. The results are identical ,so it indicates that area wind measurement is of great practical application value.

关 键 词：单经纬仪测风 基线测风 面积测风 

分 类 号：P412.2[天文地球—大气科学及气象学]