一种应用于卫星热红外遥感的透过率简化辐射传输计算方案

A Simplified Radiative Transfer Calculation Scheme for Transmittance in Satellite Thermal Infrared Remote Sensing

  • 摘要: 热红外大气辐射传输会受到各种因素的影响,大气透过率是其中一个重要参量。目前,对于热红外谱段(8~14 μm)上大气透过率的研究仍然面临着背景参数输入过多且不易获取的问题。基于此,提出了一种应用于卫星热红外遥感的大气透过率简化辐射传输计算方案。利用MODTRAN模型对大气透过率的影响参数进行整体定量模拟分析,从而得到影响大气透过率的关键参数,由此形成一套基于MODTRAN模型的参数简化方案。在MERSI-Ⅱ两个热红外通道的中心波长处,对MODTRAN模型和参数简化方案计算出的大气透过率做对比验证,R2均大于0.99,RMSE最大为0.007458,具有较高精度。参数简化方案仅依赖于观测天顶角和水汽柱浓度,不需要CO2、O3和气溶胶光学厚度。相比于MODTRAN模型,参数简化方案输入参数减少了,计算效率也随之提高。本研究为热红外数据大气校正提供了理论支撑。

     

    Abstract: Atmospheric radiative transfer in the thermal infrared spectrum is influenced by various factors, and atmospheric transmittance is a critical parameter. Currently, researching atmospheric transmittance within 8-14 μm thermal infrared spectrum remains challenging because of numerous elusive input background parameters. Consequently, a simplified parameterization scheme for thermal infrared radiative transfer in satellite remote sensing is proposed. Using the moderate resolution atmospheric transmission (MODTRAN) model, the impact parameters of atmospheric transmittance were quantitatively simulated and analyzed, to identify key parameters, leading to the development of a MODTRAN-model-based simplified scheme. Atmospheric transmittance values calculated by the MODTRAN model and simplified scheme were compared and validated at the central wavelengths of the two thermal infrared channels of a medium resolution spectral imager-LL (MERSI-LL). The R2 value exceeded 0.99, and the root mean-square error (RMSE) was below 0.007458, indicating high accuracy. The simplified scheme relies solely on the view zenith angle and water vapor column, eliminating the need for CO2, O3, and aerosol optical depth. Compared with the MODTRAN model, the simplified scheme reduces the number of input parameters and enhances computational efficiency. This study offers theoretical support for atmospheric correction of thermal infrared data.

     

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