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Measurements of atmospheric turbulence with the dual-beamwidth method using the MST radar at Gadanki, India

机译:在印度Gadanki的MST雷达采用双波束宽度法测量大气湍流

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摘要

A brief experiment was conducted during 24-29 April and 9-10 May 2002,using the MST radar at Gadanki, India, to test the dual-beamwidth method ofestimating the turbulence kinetic energy (TKE). Because the beamwidth can bemodified on only one polarization at a time at Gadanki, an elliptical beamwas used with a modified dual-beamwidth analysis. Estimates of the TKE fromthe dual-beamwidth method and the traditional method are very similar inregions of light winds (~10ms). In regions of stronger wind(~15ms) the traditional method often gives TKE0 becausethe beam-broadening correction is greater than the observed spectral width.It is suggested that some of the problems with the traditional method aredue to the uncertainty in the effective width of the radar beam. In all regionsthe modified dual-beamwidth method gives TKE0 on the beam parallel to theprevailing wind; on this beam the estimates depend only on the ratio of thebeamwidths, which is presumably well-known, and the observed spectralwidths. The values of TKE from the dual-beamwidth method are approximatelyconstant with height at 0.2ms from about 5 to 7.5km duringthe afternoon during both April and May (all April observations were madebetween 9:00 and 17:00 local time), and then decrease rapidly to about 0.02msby about 9km. The data from May extend over one fulldiurnal period and the diurnal range of TKE during this period is found tobe about 5dB below about 12km and from about 15 to 19km, near thetropopause, with maximum values during local afternoon.
机译:在印度Gadanki的MST雷达于2002年4月24日至29日和5月9日至10日进行了一个简短的实验,以测试估计湍流动能(TKE)的双束宽方法。由于在Gadanki上一次只能在一个偏振上修改光束宽度,因此使用椭圆光束进行修改的双光束宽度分析。根据双束宽度方法和传统方法对TKE的估计在小风(<〜10ms)区域非常相似。在强风(>〜15ms)区域中,传统方法通常使TKE <0,因为光束扩展校正大于观察到的光谱宽度。建议使用传统方法的一些问题是由于有效方法的不确定性雷达波束的宽度。在所有区域中,改进的双束宽度方法在平行于盛行风的波束上使TKE> 0;在此光束上,估计仅取决于大概众所周知的光束宽度的比率以及观察到的光谱宽度。在4月和5月的下午,双束宽度方法的TKE值大致恒定,高度为0.2ms,从大约5 km到7.5 km(4月的所有观测值均在当地时间9:00至17:00之间),然后降低迅速上升到约0.02毫秒乘以约9公里。从5月份开始的数据延续了一个完整的昼夜周期,在这段时间内,TKE的昼夜范围在对流层顶附近约12公里以下约5dB,从约15至19公里,在当地下午达到最大值。

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