Global, spatially explicit modelling of zenith wet delay with XGBoost

被引:2
|
作者
Crocetti, Laura [1 ]
Schartner, Matthias [1 ]
Zus, Florian [2 ]
Zhang, Wenyuan [1 ,3 ]
Moeller, Gregor [1 ,4 ]
Navarro, Vicente [5 ]
See, Linda [6 ]
Schindler, Konrad [1 ]
Soja, Benedikt [1 ]
机构
[1] Swiss Fed Inst Technol, Inst Geodesy & Photogrammetry, CH-8093 Zurich, Switzerland
[2] GeoForschungsZentrum GFZ, Dept Geodesy, Telegrafenberg, D-14473 Potsdam, Germany
[3] China Univ Min & Technol, Sch Environm Sci & Spatial Informat, 1, Daxue Rd, Xuzhou 221116, Jiangsu, Peoples R China
[4] TU Wien, Dept Geodesy & Geoinformat, Wiedner Hauptstr 8-10, A-1040 Vienna, Austria
[5] European Space Agcy ESA, Nav Sci Off, Camino Bajo Castillo, Villanueva De La Canada 28692, Madrid, Spain
[6] Int Inst Appl Syst Anal IIASA, Novel Data Ecosyst Sustainabil Res Grp, Schlossplatz 1, A-2361 Laxenburg, Lower Austria, Austria
关键词
Zenith wet delay (ZWD); Global predictions; XGBoost; Machine learning (ML); GNSS;
D O I
10.1007/s00190-024-01829-2
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Radio signals transmitted by Global Navigation Satellite System (GNSS) satellites experience tropospheric delays. While the hydrostatic part, referred to as zenith hydrostatic delay (ZHD) when mapped to the zenith direction, can be analytically modelled with sufficient accuracy, the wet part, referred to as zenith wet delay (ZWD), is much more difficult to determine and needs to be estimated. Thus, there exist several ZWD models which are used for various applications such as positioning and climate research. In this study, we present a data-driven, global model of the spatial ZWD field, based on the Extreme Gradient Boosting (XGBoost). The model takes the geographical location, the time, and a number of meteorological variables (in particular, specific humidity at several pressure levels) as input, and can predict ZWD anywhere on Earth as long as the input features are available. It was trained on ZWDs at 10718 GNSS stations and tested on ZWDs at 2684 GNSS stations for the year 2019. Across all test stations and all observations, the trained model achieved a mean absolute error of 6.1 mm, respectively, a root mean squared error of 8.1 mm. Comparisons of the XGBoost-based ZWD predictions with independently computed ZWDs and baseline models underline the good performance of the proposed model. Moreover, we analysed regional and monthly models, as well as the seasonal behaviour of the ZWD predictions in different climate zones, and found that the global model exhibits a high predictive skill in all regions and across all months of the year.
引用
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页数:19
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