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Initial Observations for Precipitation Cores With X-Band Dual Polarized Phased Array Weather Radar

机译:X频段双极化相控阵天气雷达初始观察沉淀核心

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The first X-band dual polarized phased array weather radar (DP-PAWR), which simultaneously transmits pulses of horizontal and vertical polarized radiation, was developed and installed at Saitama University, Japan, in December 2017. The DP-PAWR uses mechanical and electronic scanning at azimuth and elevation angles, respectively. It provides polarimetric precipitation measurements via 3-D volume scanning with an update rate between 10 and 60 s, for a range of up to 80 km. Here, we describe the initial DP-PAWR observation results. To evaluate the DP-PAWR observation accuracy, we compared the observational data with radar variables derived from Parsivel disdrometer data. In comparison with the disdrometer, the relative observation accuracy for the DP-PAWR radar reflectively factor had a standard deviation of 1.1 dB and mean value of 0.4 dB. We also conducted detailed observations of a developing thunderstorm using a specific differential phase ( $K_{mathrm {dp}}$ ) column, focusing on the $K_{mathrm {dp}}$ core during the storm. The $K_{mathrm {dp}}$ core movements provided useful information about the convection flow during the storm.
机译:同时发射水平和垂直偏振辐射的脉冲的第一X频段双极化相控阵天气雷达(DP-PAWR),并在日本埼玉大学,2017年12月开发并安装了水平大学。DP-PAWR使用机械和电子分别扫描方位角和高度角度。它通过3-D体扫描提供极化降水测量,更新速率在10到60秒之间,范围高达80公里。在这里,我们描述了初始DP-PAWR观察结果。为了评估DP-PAWR观察精度,我们将观察数据与来自Parsivel Discrometer数据的雷达变量进行比较。与Discrometer相比,DP-PAWR雷达反射因子的相对观察精度具有1.1dB的标准偏差,平均值为0.4 dB。我们还使用特定差异阶段进行了开发雷暴的详细观察($ k _ { mathrm {dp}}列),专注于风暴期间$ k _ { mathrm {dp}} $ core。 $ k _ { mathrm {dp}} $核心运动提供了有关风暴期间对流流程的有用信息。

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