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Diurnal variation of atmospheric water vapor based onGPS observations over Taiwan

机译:基于台湾地区GPS观测的大气水汽日变化

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Diurnal variations in the atmospheric vapor atrnBanchiao of Taiwan are studied by analyzing 30 min-averagedrndata in the summer of 1998. The surface meteorologicalrnmeasurements were mainly obtained from the Central WeatherrnBureau (CWB) of Taiwan. It is found that precipitable waterrn(PW) is increased in the afternoon. The maximum ofrnprecipitable water appears at around 0900 LST. The diurnalrnrange of precipitable water is larger on the days with thanrnwithout rainfall events. Rainfall events often occur in thernafternoon and early morning. We also examine the differencernin the characteristics of the PW signatures with and withoutrnrainfall according to the occurrence of the times for the rainfallrnpeak and the onset of rainfall.
机译:通过分析1998年夏季30分钟的平均数据,研究台湾大气层Banchiao的昼夜变化。地表气象测量主要来自台湾中央气象局(CWB)。结果发现,下午的降水量增加。最大可沉淀水出现在0900 LST附近。在没有降雨的情况下,可降水量的日变化幅度较大。降雨事件通常发生在下午和清晨。我们还根据降雨峰值时间的出现和降雨的开始,研究了有无降雨的PW信号特征的差异。

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