FY2D靜止氣象衛星OLR反演模式
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國家衛星氣象中心FY2D靜止氣象衛星地面應用系統工程資助


OLR Inverse Model for Geostationary Meteorological Satellite FY2D
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    摘要:

    介紹FY2D衛星OLR反演模式的建立過程以及模式與NOAA衛星OLR反演模式的相互對比,包括:地球大氣紅外輻射傳輸方程,全球3812條大氣廓線的大氣頂射出輻射率、射出長波輻射通量密度的模擬計算,3812條廓線FY2D窗區通道1、2、水汽通道的通道輻射率模擬計算, 通道輻射率的臨邊變暗訂正關系式的確立、3個通道波段的窄波段輻射通量密度的模擬計算。通過3812條廓線的窄波段輻射通量密度與OLR的XY坐標散點圖,建立OLR回歸關系式;并通過NOAA17 AVHRR通道5 OLR反演模式與FY2D窗

    Abstract:

    A primary description is made of the process of establishing the FY2D OLR inverse model, and the model comparison is conducted between NOAA and FY2D. The earthatmosphere infrared radiation transfer equation is introduced. The radiances and OLR at the top of atmosphere for 3812 sounding profiles, the channel radiance for FY2D window channel 1, 2 and water vapor channel, and the narrowband radiative flux of three FY2D channels for 3812 soundings are calculated, and the limbdarken correction equations for the 3 channel radiances are established. The FY2D OLR inverse model is devised based on the narrowband flux and OLR scattering graphs for 3812 soundings. By comparing the NOAA17 AVHRR channel 5 OLR inverse model with the FY2D window channel 2 OLR inverse model, it is concluded that the two satellites OLR inverse models are nearly the same. An example of the FY2D OLR product and the product quality examination is also given.

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吳曉. FY2D靜止氣象衛星OLR反演模式[J].氣象科技,2008,36(5):634~638

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  • 收稿日期:2007-07-10
  • 定稿日期:2007-10-12
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