FY-3D卫星MERSI-Ⅱ热红外通道劈窗仿真计算简化方法

Simplified Calculation Method of FY-3D Satellite MERSI-Ⅱ Thermal Infrared Channel Split-Window Simulation

  • 摘要: 劈窗算法广泛应用于多种卫星载荷的地表温度反演。在拟合劈窗算法系数时,大量的数据迭代模拟往往非常耗时、效率低下。因此,开发一种高效率的劈窗仿真计算简化方法具有重要意义。本文首先利用MODTRAN模拟分析背景参数的变化对总辐亮度的影响,然后在FY-3D MERSI-Ⅱ两个相邻的热红外通道下,对关键参数与总辐亮度的关系进行模拟分析,并探究关键参数耦合情形下总辐亮度的变化规律。通过仿真结果可知,在MERSI-Ⅱ热红外通道下,地表温度的变化对总辐亮度的影响大于地表发射率;大气水汽含量对总辐亮度的影响程度随着地表发射率和地表温度的增大而增大,而地表发射率和地表温度对总辐亮度的影响程度随着大气水汽含量的增大而减小;在确定劈窗算法系数时,可以通过缩小大气水汽含量的取值范围来减少仿真次数,从而提高仿真效率。当地表温度在300~320 K时,大气水汽含量的取值范围为0.5~5.5 g/cm2;当地表温度在270~300 K时,大气水汽含量的取值范围缩小为0.5~4.0 g/cm2。节省的仿真次数占总次数的比例为18.23%,仿真时间缩短了26 min。简化前后方案的劈窗系数拟合和绝对差值计算结果表明,简化方案对拟合结果的影响较小。

     

    Abstract: The split-window algorithm has been widely applied for surface temperature inversion of various satellite payloads. The iterative simulation of large datasets during the fitting of split-window algorithm coefficients is often time-consuming and inefficient. Therefore, it is important to develop a highly efficient simplification method for split-window simulation computations. MODTRAN was to simulate and analyze the impact of variations in background parameters on total radiance. Subsequently, we performed a simulation analysis of the relationship between key parameters and total radiance under two adjacent thermal infrared channels of FY-3D MERSI-Ⅱ, exploring the variation patterns of total radiance under different coupling scenarios of these key parameters. Simulation results reveal that under the MERSI-Ⅱ thermal infrared channels, changes in land surface temperature have a greater impact on total radiance than surface emissivity. The effect of the atmospheric water vapor content concentration on the total radiance increases with an increase in both the land surface emissivity and land surface temperature, whereas the influence of the land surface emissivity and land surface temperature on the total radiance decreases as the atmospheric water vapor content concentration increases. When determining the coefficients for the split-window algorithm, narrowing the range of the atmospheric water vapor content concentration can reduce the number of simulations required, thereby enhancing the efficiency. For land surface temperatures ranging from 300 to 320 K, the atmospheric water vapor content concentration should be within 0.5 to 5.5 g/cm²; for temperatures ranging from 270 to 300 K, this range narrows to 0.5 to 4.0 g/cm². The saved simulation runs account for 18.23% of the total number of runs, which reduces the simulation time by 26 min. A comparison of the split-window coefficient fitting and absolute difference calculation results before and after simplification shows that the simplified scheme has minimal impact on the fitting outcomes.

     

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