窄带卫星辐照度物理反演太阳表面辐照度方案的验证

H. Deneke, A. Feijt, A. Lammeren, C. Simmer
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引用次数: 30

摘要

摘要提出了一种利用卫星测量的0.63 μm反射率反演下坡太阳表面辐照度的算法,该算法明确地考虑了云光学深度和综合水汽的变化。为了验证,使用了荷兰40 356个高温计测量数据和1450个NOAA-14先进甚高分辨率辐射计(AVHRR)卫星场景的长期数据集。发现卫星获取的辐照度平均高估了7%,这与许多其他研究一致,这些研究报告了由辐射传输方案计算的大气透过率与测量值相比的正偏差。这种偏差可以用AVHRR和pyranometer的校准和测量不确定度来解释。当在反演中假设水云时,发现太阳天顶角对偏差有很强的依赖性。在冰云中没有观察到这种依赖关系。目前,没有足够的资料对……作出结论性的解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Validation of a Physical Retrieval Scheme of Solar Surface Irradiances from Narrowband Satellite Radiances
Abstract An algorithm is presented to derive the downwelling solar surface irradiance from satellite measurements of the 0.63-μm reflectance, which explicitly accounts for variations in cloud optical depth and integrated water vapor. For validation, a long-term dataset of 40 356 pyranometer measurements and 1450 NOAA-14 Advanced Very High Resolution Radiometer (AVHRR) satellite scenes of the Netherlands is used. A mean overestimate of the satellite-retrieved irradiance by 7% is found, which is consistent with numerous other studies reporting positive biases of atmospheric transmissivities that are calculated by radiative transfer schemes in comparison with measurements. The bias can be explained by the calibration and measurement uncertainties of both the AVHRR and pyranometer. A strong solar zenith angle dependence of the bias is found when water clouds are assumed in the retrieval. Such a dependence is not observed for ice clouds. Currently, there is not enough information for a conclusive explanation o...
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