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Variations of the Precipitation Water Vapor By Using GPS Data Triggered Raining in The Summer of Thailand

机译:通过使用GPS数据在泰国夏天下雨的沉淀水蒸气的变化

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The variation of water vapor can be detected from the Global Positioning System (GPS) data. The GPS signal was delayed when propagated through the wet atmosphere. The delayed signal can be retrieved into Precipitation Water Vapor (PWV) data. The GPS data of CUSV station from 2009 to 2012 were used in this research. The results showed that the PWV varied during the summer of Thailand. The PWV were slightly increased from 20 mm at the beginning of the season to 40 mm at the end of season. The increased PWV data were shown as linear line. A slope of the linear line may relate with the amount of the cumulative rain in the season. The steeper line might relate to the great number of raining in the end of the season, otherwise, the fairly gradual line might relate to the raining at any time in the season. The high level of PWV up to around 33 mm could induce the rain in the summer of Thailand.
机译:可以从全球定位系统(GPS)数据中检测水蒸气的变化。当通过湿气氛传播时,GPS信号被延迟。可以将延迟信号检索到沉淀水蒸气(PWV)数据中。在本研究中使用了2009年至2012年CUSV站的GPS数据。结果表明,泰国夏天的PWV变化。在季节开始到季节结束时,PWV略微增加到40毫米。增加的PWV数据显示为线性线。线性线的斜率可能与季节累积雨量有关。陡峭的线可能与赛季结束时的大量下雨有关,否则,相当渐进的线路可能与赛季随时下雨。高达约33毫米的高水平可能会在泰国的夏天诱导雨。

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