Hu Xiuqing, Huang Yibin, Lu Qifeng, et al. Retrieving precipitable water vapor based on the near-infrared data of FY-3A satellite. J Appl Meteor Sci, 2011, 22(1): 46-56.
Citation: Hu Xiuqing, Huang Yibin, Lu Qifeng, et al. Retrieving precipitable water vapor based on the near-infrared data of FY-3A satellite. J Appl Meteor Sci, 2011, 22(1): 46-56.

Retrieving Precipitable Water Vapor Based on the Near-infrared Data of FY-3A Satellite

  • Received Date: 2009-12-28
  • Rev Recd Date: 2010-09-26
  • Publish Date: 2011-02-28
  • The technique of retrieving precipitable water vapor (PWV) based on near-infrared (NIR) data of Medium Resolution Spectral Imager (MERSI) on board FY-3A satellite is introduced. Five NIR channels are designed on the MERSI instrument for PWV observation, three of which are water vapor absorption channels centered near 905 nm, 940 nm and 980 nm respectively and others are atmospheric window channels at 865 nm and 1030 nm. The method adopted here for PWV retrieval is based on the ratio of reflected solar radiance (or apparent reflectance) detected by satellite between water vapor absorption channels and atmospheric window channels. By employing channel ratios, the aerosol extinction distribution and the variation effect of surface reflectance are partially removed, and the atmospheric transmittance of water vapor channels is approximately obtained. The PWV is derived from the atmospheric transmittance based on a Look-up Table which is pre-calculated using a radiation transfer model. The sensitivities of atmospheric transmission in each NIR water vapor channels of MERSI to the total precipitable water vapor are also simulated. It is found that 905 nm channel is more sensitive under humid conditions while the strong absorption channel at 940 nm is sensitive under dry conditions. And the two weak absorption channels have similar sensitivity to total water vapor amount. In this case, under a given atmosphere condition, the derived PWV values from three water vapor channels may be a little different. The weighted average of three derived PWV values is regarded as the final PWV product and the weighing coefficients are determined by their sensitivity.The procedure of the operational PWV product generation is designed and conducted for experimental retrieval. Based on the global data of MERSI, FY-3A Products Generation System (PGS) can successfully generate the daily global and regional PWV L2 products and multi-day integrated L3 products, which can clearly display the spatial distribution of water vapor amounts over global land area. The result indicates that FY-3A/MERSI has an excellent ability in detecting NIR water vapor, and can demonstrate fine characteristic of PWV spatial distributions. As 940 nm channel shows good application under dry atmosphere conditions and 905 nm or 980 nm channel work well under humid situation, acceptable retrieval accuracy can always be achieved by combining these channels. In order to assess the accuracy, the retrieved PWV from MERSI NIR are compared with the ground-based sounding data. Over cloud free area, there is a good agreement between them in variation trend and spatial distribution. The MERSI PWV results are steady but 20%—30% lower than sounding, so the retrieval algorithm and the Look-up Table need to be updated to reduce this bias in the near future.
  • Fig. 1  The comparison of spectral location of the NIR channels between FY-3A/MERSI and EOS/MODIS

    Fig. 2  Look-up Table (LUT) establishment of PWV and retrieval procedure

    Fig. 3  The dependence of the transmission ratio between two channels of FY-3A/MERSI on the water vapor amount

    Fig. 4  Cases of MERSI PWV product over land (a) granule product in five minutes (RGB true color image), (b) granule product in five minutes (retrieved results), (c) daily Chinese regional product on 27 August 2009, (d) daily global product on 18 Apr 2009, (e) multi-day composition product

    Fig. 5  The distribution of PWV from ground-based radio-sosunding on 27 August 2009 (unit: g·cm-2)

    Fig. 6  A comparison of NIR retrieved PWV from FY-3A/MERSI with the ground-based radio-sounding data in August and December of 2009 (unit: g·cm-2)

    Fig. 7  A comparison of NIR PWV between MERSI and MODIS on 16 December 2008 (a) MODIS, (b) MERSI

    Table  1  The spectral location and width of NIR channels of different satellite remote sensors at water vapor absorption spectral range (unit:nm)

    仪器通道 FY-1C (1D)/MVISR SZ-3/CMODIS FY-3A/MERSI EOS/MODIS
    中心波长 宽度 中心波长 宽度 中心波长 宽度 中心波长 宽度
    水汽通道 905 20 905 20 905 30
    936 50 925 20 940 20 936 10
    945 20 980 20 940 50
    965 20
    985 20
    两侧窗区通道 865 50 865 20 865 20 865 40
    1005 20 1030 20 1240 20
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    Table  2  The specification of MERSI PWV over land

    产品类型 投影方式 覆盖范围 空间分辨率 数据量/Mbyte 生成频次
    5 min段产品 无投影 5 min轨道 1 km×1 km 59 5 min 1次
    日产品 等经纬度 全球 0.05°×0.05° 74.1 每日1次
    中国区域日产品 等经纬度 5°~55°N, 70°~140°E 0.01°×0.01° 300 每日1次
    旬产品 等经纬度 全球 0.05°×0.05° 74.1 每旬1次
    月产品 等经纬度 全球 0.05°×0.05° 74.1 每月1次
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    • Received : 2009-12-28
    • Accepted : 2010-09-26
    • Published : 2011-02-28

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