伽丽丽, 魏合理, 徐青山, 陈秀红. 中国区域940nm带整层大气水汽透过率的参数化模式[J]. 武汉大学学报 ( 信息科学版), 2011, 36(2): 204-207.
引用本文: 伽丽丽, 魏合理, 徐青山, 陈秀红. 中国区域940nm带整层大气水汽透过率的参数化模式[J]. 武汉大学学报 ( 信息科学版), 2011, 36(2): 204-207.
QIE Lili, WEI Heli, XU Qingshan, CHEN Xiuhong. Parametrization of Total Atmospheric Absorbing Transmittances by Water Vapor at 940 nm in China[J]. Geomatics and Information Science of Wuhan University, 2011, 36(2): 204-207.
Citation: QIE Lili, WEI Heli, XU Qingshan, CHEN Xiuhong. Parametrization of Total Atmospheric Absorbing Transmittances by Water Vapor at 940 nm in China[J]. Geomatics and Information Science of Wuhan University, 2011, 36(2): 204-207.

中国区域940nm带整层大气水汽透过率的参数化模式

Parametrization of Total Atmospheric Absorbing Transmittances by Water Vapor at 940 nm in China

  • 摘要: 用MODTRAN模拟计算了全国34个地点的逐月和全年平均大气模式在940 nm波段的水汽透过率,并拟合出每种大气模式水汽透过率与水汽量经验关系式中的参数a、b。结果表明,参数a、b值与模式的整层大气可降水量有较好的相关性,并建立了a-W、b-W的经验关系式,且该关系式与海拔高度H(地面气压p0)有关。最后分析了a、b值的变化对地基消光反演水汽量精度的影响。

     

    Abstract: The water vapor transmittances in the 940 nm band are computed using MODTRAN for 34 sites in China.Parameters a and b for all the atmospheric models in the empirical water vapor transmittance function are fitted.It is found that the values of a and b is the function of atmospheric water vapor amount.The empirical functions are established for the relationships between the values of a and b and atmospheric model's perciptible water.Considering the parameter of the surface altitude H(or surface pressure p0),the empirical coefficients related to H are parameterized.Finally,the uncertainty in retrieved PWV caused by parameter a and b is analyzed.

     

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