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中国西南地区GPS大气水汽转换系数模型精化研究
引用本文:黄良珂,吴丕团,王浩宇,刘立龙.中国西南地区GPS大气水汽转换系数模型精化研究[J].大地测量与地球动力学,2019,39(3):256-261.
作者姓名:黄良珂  吴丕团  王浩宇  刘立龙
作者单位:桂林理工大学测绘地理信息学院,桂林市雁山街319号,541004;广西空间信息与测绘重点实验室,桂林市雁山街319号,541004;广西壮族自治区地理信息测绘院,广西壮族自治区柳州市东环大道10号,545006
基金项目:国家自然科学基金;国家自然科学基金;广西八桂学者岗位专项;广西自然科学基金;广西自然科学基金;广西空间信息与测绘重点实验室开放基金;广西空间信息与测绘重点实验室开放基金
摘    要:利用中国西南地区19个探空站2011~2014年数据,通过积分法计算大气水汽转换系数K。采用2011~2013年的K值对Emardson模型进行精化,分别构建西南地区不顾及和顾及高程因子的K值模型Emardson-I和Emardson-H。利用2014年积分计算的K值检验这两种模型的预报精度,结果表明:1)相对于Emardson-I模型,Emardson-H模型表现出更高的K值预报精度和更好的适应性;2)在高海拔地区,Emardson-H模型预报精度明显优于Emardson-I模型,表明高程因子是影响高海拔地区K值计算的重要因素。将两种新模型用于拉萨站GPS大气水汽反演,Emardson-H模型表现出更优的反演精度,两种模型的反演精度均优于2 mm。

关 键 词:西南地区  GPS大气水汽  转换系数  模型精化

Refining the GPS Atmospheric Water Vapor Conversion Factor Model over Southwest China
HUANG Liangke,WU Pituan,WANG Haoyu,LIU Lilong.Refining the GPS Atmospheric Water Vapor Conversion Factor Model over Southwest China[J].Journal of Geodesy and Geodynamics,2019,39(3):256-261.
Authors:HUANG Liangke  WU Pituan  WANG Haoyu  LIU Lilong
Institution:(College of Geomatics and Geoinformation,Guilin University of Technology,319 Yanshan Street,Guilin 541004,China;Guangxi Key Laboratory of Spatial Information and Geomatics,319 Yanshan Street,Guilin 541004,China;Institute of Geoinformation and Geomatics of Guangxi Zhuang Autonomous Region,Liuzhou 545006,China)
Abstract:The atmospheric water vapor conversion factor K is an important parameter in the progress of retrieving precipitable water vapor(PWV) from the zenith wet delay(ZWD) of the GPS. In this paper, four years of atmospheric water vapor conversion factor K values are calculated using radiosonde profiles derived from 19 radiosonde stations distributed in southwest China. The Emardson model is refined using K values from 2011 to 2013; finally, two refined K factor models are developed: the Emardson-I model(elevation independent) and the Emardson-H model(elevation dependent). These two new models are validated using 2014 K values. The results are:(1) Emardson-H model yields more accurate and stable results than Emardson-I model for predicting the K factor; (2) the performance of the Emardson-H model is significantly better than the Emardson-I model in high-altitude areas, indicating that elevation is an important factor for the K value calculation in these areas. In addition, the two new models are used for retrieving GPS-PWV at Lhasa station, with results showing that the Emardson-H model has excellent performance in retrieving GPS-PWV, and both models can achieve GPS-PWV retrieval precision of better than 2 mm.
Keywords:southwest China  GPS precipitable water vapor  conversion factor  model refinement  
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