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    泰山C波段与济南S波段双偏振雷达强降水型飑线探测差异性分析

    Analysis of difference in detection of strong precipitation squall line between Taishan C-band dual polarization radar and Jinan S-band dual polarization radar

    • 摘要: 为探究泰山C波段双偏振雷达(CDD)与济南S波段双偏振雷达(SAD)对强降水型飑线的探测差异,选取山东省2022年10月2日和2023年6月27日两次强降水型飑线过程,结合常规气象资料及雷达探测资料对重合观测区域回波强度、差分反射率(ZDR)及概率密度等特征进行对比分析。结果表明:两部雷达对飑线回波强度和ZDR的探测有明显差别,飑线强度越强,两部雷达的探测差异越大,CDD探测到的反射率因子低值明显偏多而高值明显偏少,较强飑线可能会出现更多的ZDR负值;在3 km高度处CDD的ZDR具有更多大于4 dB的高值,主要是由尺寸较大的液态粒子造成;两部雷达的回波强度和ZDR差异均随着高度增加而降低,高层CDD的探测值可信度较高,可以较好地捕捉到飑线的云微物理特征;CDD海拔较高,有利于对高层云的探测,通过与SAD对比发现虽然出现了回波强度偏弱、强回波后的衰减、双偏振特征虚假度较高等问题,但也能够显示强降水阶段的特征差异,因此两部雷达组网可以有效提高SAD高层盲区观测能力。

       

      Abstract: In order to investigate the detection differences between Taishan C-band radar (CDD) and Jinan S-band radar (SAD) on the strong precipitation squall line,two strong precipitation squall line processes in Shandong Province on October 2,2022 and June 27,2023 are selected,and the characteristics of echo intensity,differential reflectivity (ZDR) and probability density of the overlapping observation area are compared and analyzed with the conventional meteorological data and radar data.The results show that there are significant differences in the detection of squall line echo intensity and ZDR between the two radars,and the stronger the squall line,the greater the difference in detection between the two radars.low values of reflectivity factor detected by the CDD are significantly more and high values are significantly less.Stronger squall lines may have more negative ZDR values.The ZDR of the CDD at 3 km altitude has more high values of more than 4 dB,which is mainly caused by the liquid particles with larger sizes.The echo strength and ZDR differences of both radars decrease with increasing altitude,and the detection values of the CDD at higher altitudes have higher confidence in capturing the cloud micro-physical features of the squall line better.The higher altitude of the CDD is conducive to the detection of high-level clouds,and the comparison with the SAD reveals that although there are problems such as weak echo strength,attenuation after strong echoes,and high false degree of double polarization features,it can also be able to show the feature differences in the stage of strong precipitation,and thus the two radars can effectively improve the observation capability of the SAD in the high-level blind zone.

       

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