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Validation of the 1290 MHz wind profiler at Payerne, Switzerland, using radiosonde GPS wind measurements

机译:使用无线电探空仪GPS风力测量结果验证瑞士Payerne的1290 MHz风力剖面仪

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摘要

The validation of a 1290 MHz wind profiler using 3 years of collocated wind profiler and radiosonde wind measurements is presented. The radiosonde wind information is derived from global positioning system data and is vertically averaged to match the vertical resolution of the wind profiler measurements. The integration period of the wind profiler is chosen such that it is centred around the radiosonde measurement time. Periods where bird migration must be expected have been systematically excluded. The standard deviation of the differences between wind profiler and radiosonde in the wind components u and v is between 1.75 and 2 m s(-1) and the bias is smaller than 0.75 m s(-1) for heights below 6 km for both modes. Some part of the obtained standard deviation can be explained by the fact that radiosonde and wind profiler measurements are not representative for each other. In order to reduce the representativeness error, a subset of cases has been selected, for which the wind field was stationary during the measurement period and uniform across the sampled volume of the wind profiler. The standard deviation derived from the subset is between 1 and 1.5 m s(-1) while the bias changes only little. This reduction can be attributed to a reduction in the representativeness error and in the retrieval error of the wind profiler since atmospheric homogeneity is a basic assumption in the wind retrieval. The obtained value of 1.5 m s(-1) can be taken as an upper limit of the measurement uncertainty of the wind profiler in favourable measurement conditions.
机译:本文介绍了使用3年并置风廓线仪和探空仪风向测量仪对1290 MHz风廓线仪进行的验证。探空仪的风信息是从全球定位系统数据中得出的,并进行垂直平均以匹配风廓线仪测量的垂直分辨率。选择风廓线仪的积分周期,使其以无线电探空仪测量时间为中心。系统地排除了必须预料到鸟类迁徙的时期。两种模式下,在风分量u和v中,风廓线仪和探空仪之间差异的标准偏差在1.75和2 m s(-1)之间,并且对于低于6 km的高度,偏差小于0.75 m s(-1)。探空仪和风廓线仪的测量值不能相互代表这一事实可以解释所获得的标准偏差的某些部分。为了减少代表性误差,我们选择了一些情况的子集,这些子集的风场在测量期间是固定的,并且在风廓线仪的采样体积上是均匀的。从子集得出的标准偏差在1到1.5 m s(-1)之间,而偏差仅变化很小。这种减少可以归因于风廓线仪的代表性误差和取回误差的减少,因为大气均匀性是取风的基本假设。所获得的1.5 m s(-1)的值可以作为在有利的测量条件下风廓线仪的测量不确定度的上限。

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