Zhong Liujun, Ruan Zheng, Ge Runsheng, et al. Calibration method of echo intensity of wind profile radar. J Appl Meteor Sci, 2010, 21(5): 598-605.
Citation: Zhong Liujun, Ruan Zheng, Ge Runsheng, et al. Calibration method of echo intensity of wind profile radar. J Appl Meteor Sci, 2010, 21(5): 598-605.

Calibration Method of Echo Intensity of Wind Profile Radar

  • Received Date: 2009-12-02
  • Rev Recd Date: 2010-07-08
  • Publish Date: 2010-10-31
  • A lot of researches about wind profile radar are based on analysis of echo power. So the estimation accuracy of echo power has direct effects on the use and expansion of wind profile radar data. At present, return signal power of wind profile radar is estimated by signal to noise ratio (SNR) and radar system noise power. Environmental noise may cause errors when estimating SNR in power spectrum of wind profile radar, affecting calibration accuracy. Another viable option is quantitatively testing the receiver and signal processor respectively using the same signal source, and then the calibration curve of radar systems can be determined according to the measured signal processor linear curve. Using this method, the calibration curve of CFL 03 wind profile radar is determined, and probe data of the radar in July and August, weather radar data and surface rain gauge data are compared. The results show that the weak signal of wind profile radar can be calibrated effectively, on the basis of measurement of the coherent accumulation and pulse compression accumulation using intermediate frequency source. The method proves feasible through the actual test. And through field experiments it can be seen that calibrated echo intensity of wind profile radar and SA weather radar echo intensity are basically the same with an average error less than 2 dB, within the scope of weather radar calibration error. The errors between calibrated echo intensity of wind profile radar and ground rain gauge data is less than 2 dB, indicating that the calibration results are credible.
  • Fig. 1  Receiver system test diagram

    Fig. 2  Linear dynamic range of the receiver

    Fig. 3  Systemcalibration (a) low mode, (b) high mode

    Fig. 4  Location diagram of Guangzhou SA weather radar and wind profile radar in Dongguan with the ground rain gauge

    Fig. 5  Echo intensity of wind profile radar and weather radar (a) light rain, (b) heavy rain

    Table  1  Test of coherent accumulation

    Table  2  est of pulse compression accumulation

    Table  3  Echo intensity in sunny day in Dongguan (unit:dBZ)

  • [1]
    刘淑媛,郑永光,陶祖钰.利用风廓线雷达资料分析低空急流的脉动与暴雨关系.热带气象学报,2003,19(3):63-68. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200303007.htm
    [2]
    Boyer E,Petitdidier M,Adnet C,et al.Subapace-based Spectral Analysis for VHF and UHF Radar Signals.Proc PSIP,2001:385-390.
    [3]
    张培昌,王振会.大气微波遥感基础.北京:气象出版社,1995:100-120.
    [4]
    王令,郑国光,康玉霞,等.多普勒雷达天气雷达径向速度图上的雹云特征.应用气象学报,2006,17(3):281-287. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX200603003.htm
    [5]
    李华宏,薛纪善,王曼,等.多普勒雷达风廓线的反演及变分同化试验.应用气象学报,2007,28(1):50-57. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20070110&flag=1
    [6]
    许小峰,胡欣,王卫丹,等.国内大气科学发展状况及优先领域分析.应用气象学报,2006,17(6):657-664. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=200606114&flag=1
    [7]
    张堵昌,杜秉玉,戴铁丕.雷达气象学.北京:气象出版社,2000:70-85.
    [8]
    何平.相控阵风廓线雷达.北京:气象出版社,2006:64-89.
    [9]
    Rogers R R,Baumgardner D,Ethier S A,et al.Comparison of raindrop size distributions measured by radar wind profiler and by airplane.J Appl Meteor,1993,32(4):694-699. doi:  10.1175/1520-0450(1993)032<0694:CORSDM>2.0.CO;2
    [10]
    White A B,Gottas D J,Ralph F M,et al.An automated bright band height detection algorithm for use with Doppler radar spectral moments.J Atmos Oceanic Technol,2002,19(5):687-697. doi:  10.1175/1520-0426(2002)019<0687:AABHDA>2.0.CO;2
    [11]
    Bianco L,Wilezak J M.Convective boundary layer depth:Improved measurement by Doppler radar wind profiler using fuzzy logic methods.J Atmos Oceanic Technol,2002,19(11):1745-1758. doi:  10.1175/1520-0426(2002)019<1745:CBLDIM>2.0.CO;2
    [12]
    Angevine W M,White A B,Avery S K.Boundary layer depth and entrainment zone characterization with a boundary layer profiler.Boun-Layer Meteor,1994,68:375-385. doi:  10.1007/BF00706797
    [13]
    黄伟,张沛源,葛润生.风廓线雷达估测雨滴谱参数.气象科技,2002,30(6):334-340. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKJ200206002.htm
    [14]
    阮征,何平,葛润生.风廓线雷达对大气折射率结构常数的探测研究.大气科学,2008,32(1):133-140. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200801012.htm
    [15]
    阮征,葛润生,吴志根.风廓线仪探测降水云体结构方法的研究.应用气象学报,2002,13(5):170-179. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20020343&flag=1
    [16]
    何平,朱小燕,阮征,等.风廓线雷达探测降水过程的初步研究.应用气象学报,2009,20(4):465-470. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=200904011&flag=1
    [17]
    马建立,阮征,葛润生,等.风廓线雷达估算大气返回信号功率方法的研究.气象科技,2002,37(1):89-92.
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    • Received : 2009-12-02
    • Accepted : 2010-07-08
    • Published : 2010-10-31

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