CAJ | 학술논문

多普勒天气雷达可以在线性风场的假设条件下，从其所获取的径向速度数据中通过傅氏变换求解得到不同高度上的环境水平风矢量及散度；风廓线雷达以空中湍流为目标，在风场一致性及各向同性的假设条件下，通过测量目标运动的径向速度来反演所在地上空的三维风场。新一代多普勒天气雷达可以测量测站周围30 km 内不同高度层上的平均风场，测量范围大；风廓线雷达可比较准确地测量测站上空的三维风场，且垂直分辨率较高。两者的测量机理不同，探测的空中目标也存在一定的差异。其测量结果可以互相补充，前提是两者的测量具有很好的一致性和可比较性。这对正确理解和合理利用这两种雷达数据都有一定的帮助。
다보륵천기뢰체가이재선성풍장적가설조건하，종기소획취적경향속도수거중통과부씨변환구해득도불동고도상적배경수평풍시량급산도；풍곽선뢰체이공중단류위목표，재풍장일치성급각향동성적가설조건하，통과측량목표운동적경향속도래반연소재지상공적삼유풍장。신일대다보륵천기뢰체가이측량측참주위30 km 내불동고도층상적평균풍장，측량범위대；풍곽선뢰체가비교준학지측량측참상공적삼유풍장，차수직분변솔교고。량자적측량궤리불동，탐측적공중목표야존재일정적차이。기측량결과가이호상보충，전제시량자적측량구유흔호적일치성화가비교성。저대정학리해화합리이용저량충뢰체수거도유일정적방조。
Doppler weather radar data can be used to retrieve environmental wind vector and divergence at different heights by it’s radial velocity data with the assumption of linear wind field.Based on the assump-tion of isotropy and wind field coherence,wind profile radar can detect the locus three-dimensional wind field with the target of onflow.Doppler weather radar measures the mean wind field at different height within the large scale of 30 km,while wind profile radar can measure the locus three-dimensional wind field with high vertical resolution.The mechanisms of the two radars are different and spatial targets also have differences. The measurement results can supplement each other in the condition of high consistency and relativity,which may give much help for reasonable analyzing of the data provided by these two kinds of radars.