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Detection on the Precipitable Water Vapor during Summer Rainfall by Nanjing GPS Network

机译:南京GPS网探测夏季降水中的可沉淀水汽。

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According to the ground-based principles of GPS meteorology, utilizing on the observation data of Nanjing regional GPS network, introducing the observation data of three IGS base stations to construct very long baselines, and combining with the atmospheric parameters by surface observation, the GPS absolute precipitable water vapor (PWV) and relative PWV were estimated. Compared with SONDE PWV and the actual surface rainfall, results show that there has a good relativity between GPS PWV and SONDE PWV; according to SONDE PWV, whether the average difference or correlation coefficient, GPS absolute PWV is better than relative PWV; The variation of GPS PWV value can be an intuitive response to changes in the actual surface rainfall, and Rainfall usually occurs in 4-6 hours after the value of GPS-PWV had a rapid increase; and with the value of GPS PWV significantly rise or drop, it shows the beginning or end of the rainfall. In addition, it's useful for studying on regional changes in atmospheric water vapor with Estimating PWV by regional GPS network, and can improve the accuracy of meso-, micro-scale weather forecast.
机译:根据GPS气象学的地基原理,利用南京地区GPS网的观测数据,引入三个IGS基站的观测数据来构建很长的基线,并结合地面观测的大气参数,得出GPS绝对​​值。估计了可沉淀的水蒸气(PWV)和相对PWV。与SONDE PWV和实际地面降水量相比,结果表明GPS PWV与SONDE PWV之间具有良好的相关性。根据SONDE PWV,无论是平均差还是相关系数,GPS绝对​​PWV均优于相对PWV。 GPS PWV值的变化可能是对实际地面降雨量变化的直观响应,降雨通常在GPS-PWV值迅速增加后的4-6小时内发生;随着GPS PWV值的显着上升或下降,它显示了降雨的开始或结束。此外,它对于通过区域GPS网络估算PWV来研究大气水汽的区域变化非常有用,并且可以提高中,微尺度天气预报的准确性。

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