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Retrieval of the Change of Precipitable Water Vapor by GPS Technique

机译:利用GPS技术反演可沉淀水汽的变化。

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The feasibility of GPS precipitable water vapor (PWV) is discussed based on the comparison of Radiosonde and GPS PWV where the correlation coefficient is 0.94 and the RMS is 4.0 mm. PWV change in the Chinese mainland in 2004 is graphed with the gridding method of splines in tension, according to the GPS data of the crust monitor observation network in China, combined with relevant meteorology information. According to the distribution of the annual amount of rainfall in the country, it can be concluded that the total trend of the PWV is diminishing from the south-east coastland to the north-west inland. The PWV reaches its maximum during July and August, and the minimum is reached during January and February. According to the PWV, from high to low, all districts can be ranked as south-east coastland, the inland and the tableland.
机译:基于无线电探空仪和GPS PWV的相关系数为0.94,RMS为4.0 mm的比较,讨论了GPS可沉淀水蒸气(PWV)的可行性。根据中国地壳监测观测网的GPS数据,结合相关的气象资料,采用张力样条网格化方法绘制了2004年中国大陆的PWV变化图。根据该国年降水量的分布,可以得出结论,从东南沿海到西北内陆,PWV的总体趋势正在减少。 PWV在7月和8月达到最大值,在1月和2月达到最小值。根据PWV,从高到低,所有地区都可以列为东南沿海,内陆和高原。

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