“吉林一号”宽幅01B卫星GNSS-R数据风速反演研究

Wind Speed Retrieval Using GNSS-R Data from Jilin-1Kuanfu-01B Satellite

  • 摘要: 为了初步分析和评估“吉林一号”宽幅01B卫星全球导航卫星系统反射(global navigation satellite system-reflectometry,GNSS-R)测量数据反演海面风速的有效性和可用性,建立未标定时延多普勒相关功率峰值信噪比、归一化时延波形前沿斜率和后沿斜率反演海面风速的模型,得到了反演模型反演风速与ECMWF(European Centre for Medium-Range Weather Forecasts)风速的均方根误差。当无严格数据质量控制和数据定标时,时延⁃多普勒图(delay-Doppler map,DDM)的峰值信噪比、时延波形前沿和后沿斜率的反演风速的均方根误差分别为3.22 m/s、3.67 m/s和3.49 m/s。当控制信噪比大于-6 dB时,DDM峰值信噪比反演的风速的均方根误差满足低风速反演精度2 m/s的需求,但数据量下降为无严格数据质量控制的78.11 %;对于前沿和后沿斜率,当信噪比大于-3 dB时,均方根误差小于2 m/s,数据量下降至53.74 %。结果表明,“吉林一号”宽幅01B卫星的GNSS-R数据可用于海面风速的测量。

     

    Abstract:
    Objectives Spaceborne global navigation satellite system-reflectometry(GNSS-R) has been demonstrated to be effective in retrieving global sea surface wind speed, and many missions have been launched in orbit or planned. “Jilin-1” Kuanfu-01B satellite, as a commercial remote sensing satellite of China, equipped a GNSS-R instrument to observe Earth's physical parameters. This paper aims to preliminarily analyze and demonstrate the effectiveness and feasibility of GNSS-R data from “Jilin-1” Kuanfu-01B satellite for retrieving sea surface wind speed.
    Methods Three basic observables sensitive to wind speed, namely the delay-Doppler map (DDM) peak signal-to-noise ratio (SNR), the leading-edge slope and trailing-edge slope of the normalized delay waveform, are extracted from the DDMs of “Jilin-1” Kuanfu-01B satellite, and are used to demonstrate and assess the potential in retrieving wind speed. Three basic observables have obvious inversely proportional relationships with wind speed; therefore, an empirical exponential function is used to develop the geographic model function (GMF) between the basic observables and wind speed. Furthermore, the root mean square error (RMSE) between the retrieved wind speeds and European Centre for Medium-Range Weather Forecasts (ECMWF) data are obtained.
    Results The RMSE of the retrieved wind speed using DDM peak SNR, leading-edge slope and trailing-edge slope are 3.22 m/s, 3.67 m/s and 3.49 m/s without data quality control and data calibration. When SNR is controlled to be larger than -6 dB, the RMSE of the retrieved wind speed using the DDM peak SNR reduces to be within 2 m/s, and the useful data are 78.11 % of that without data quality control. For leading-edge slope and trailing-edge slope, when SNR threshold is -3 dB, the RMSE of retrieved wind speed is also decreased to be within 2 m/s, and the useful data reduce to 53.74 %.
    Conclusions The results show that the GNSS-R data from “Jilin-1” Kuanfu-01B satellite can be used to measure sea surface wind speed. The data used in the paper are uncalibrated, therefore, the retrieved performances are not optimal. It is a key work to calibrate the influence of transmitted power, transmission gain, and propagation path on the DDM.

     

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