Guo Wei, Yin Qiu, Du Mingbin, et al. The accuracy test of retrieved precipitation water vapor based on Beidou observations. J Appl Meteor Sci, 2015, 26(3): 346-353. DOI:  10.11898/1001-7313.20150310.
Citation: Guo Wei, Yin Qiu, Du Mingbin, et al. The accuracy test of retrieved precipitation water vapor based on Beidou observations. J Appl Meteor Sci, 2015, 26(3): 346-353. DOI:  10.11898/1001-7313.20150310.

The Accuracy Test of Retrieved Precipitation Water Vapor Based on Beidou Observations

DOI: 10.11898/1001-7313.20150310
  • Received Date: 2014-09-22
  • Rev Recd Date: 2015-01-30
  • Publish Date: 2015-05-31
  • The Beidou Navigation Satellite System is an independent system under construction in China. Observations of Beidou can be used to retrieve atmospheric precipitation water vapor (PWV) and provide information of water vapor with high precise and high real time. Beidou meteorological observation network is built by Shanghai Meteorological Bureau with PANDA (position and navigation data analysist) and M300C_GNSS, UNICORE-UB240 Beidou receivers, and the atmospheric precipitation water vapor is acquired. First, satellite data is received by Beidou meteorological observations and satellite orbit files are downloaded synchronously, and then zenith total delay (ZTD) is calculated by PANDA modules, and at last the PWV is retrieved based on surface meteorological parameters observed by automatic weather stations.Results of PWV retrieved by Beidou data (WBD) are compared with both PWV retrieved by GPS data (WGPS) and radiosonde data (WRadio), as the technology of them are mature. WGPS is retrieved by two methods: One is GAMIT (GPS at MIT) with the method of double difference phase observation, the other is PANDA with the method of precise point positioning. WRadio is retrieved by the method of water vapor integration from different pressure levels. The horizontal distance difference between corresponding observations is no more than 10 km, the elevation difference between GPS and Beidou observations is no more than 5 m, and the elevation difference between radiosonde and Beidou observations is about 30 m. Results show that the root mean square error (RMSE) between WBD and WGPS is no more than 3.5 mm, the correlation coefficient between them is over 0.95, and the RMSE between WBD and WGPS-P is smaller than that between WBD and WGPS-G, which means that the retrieve method has certain influence on results of PWV. The RMSE between WBD and WGPS-Radio is about 3.6 mm, the correlation coefficient between them is over 0.96, and WBD is on the high side compared with WGPS-Radio. WBD can well reflect the temporal changing characteristics of water vapor in the atmosphere and has corresponding relations with precipitation, which plays an important role in short-term weather forecast and climate analysis. The accuracy of WBD relies much on the precise ephemeris of Beidou.With the development of the Beidou Navigation Satellite System, the accuracy of PWV based on Beidou observations can surpass that based on GPS observations. Therefore, making the best of the Beidou Navigation Statellite System and improving meteorological service with WBD is important for the modernization of meteorology.
  • Fig. 1  Flow diagram of calculating PWV based on Beidou data

    Fig. 2  Map of sites

    Fig. 3  Scatter plot of WGPS and WBD calculated at Lingang

    (a)WGPS calculated by GAMIT, (b)WGPS calculated by PANDA

    Fig. 4  Scatter plot of WGPS and WBD calculated at Jinshan

    (a)WGPS calculated by GAMIT, (b)WGPS calculated by PANDA

    Fig. 5  Scatter plot of WBD calculated at Luojing and WRadio calculated at Baoshan

    Fig. 6  Sequence chart of PWV at Lingang in Mar 2014

    (columnar represents corresponding rainfall, the continuous section shows lack of monitoring, black line represents the threshold for rainfall at Lingang)

    Fig. 7  Sequence chart of PWV at Baoshan in Apr 2014

    (columnar represents corresponding time rainfall, the continuous section shows lack of monitoring, black line represents the threshold for rainfall at Baoshan)

    Table  1  Information of Beidou satellite on-orbit

    卫星种类 卫星编号
    地球静止轨道卫星 G1,G3,G4,G5,G6
    倾斜地球同步
    轨道卫星
    IGSO1,IGSO2,IGSO3,
    IGSO4,IGSO5
    中圆地球轨道卫星 M3,M4,M5,M6
    DownLoad: Download CSV

    Table  2  Statistical results of WBD, WGPS and WRadio

    站点 对比方式 样本量 均方根误差/mm 平均偏差/mm 相关系数
    南汇北斗站与南汇GPS站 WBDWGPS-G 734 2.90 1.21 0.9588
    WBDWGPS-P 734 2.77 1.09 0.9698
    遥感中心北斗站与莘庄GPS站 WBDWGPS-G 657 3.43 1.05 0.9531
    WBDWGPS-P 657 3.28 0.97 0.9762
    临港北斗站与临港GPS站 WBDWGPS-G 1849 3.44 -1.18 0.9577
    WBDWGPS-P 1849 2.89 1.44 0.9748
    金山北斗站与金山GPS站 WBDWGPS-G 1382 3.24 -0.47 0.9502
    WBDWGPS-P 1382 3.15 1.75 0.9664
    罗泾北斗站与宝山探空站 WBDWRadio 127 3.64 1.24 0.9624
    DownLoad: Download CSV
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    • Received : 2014-09-22
    • Accepted : 2015-01-30
    • Published : 2015-05-31

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