Choice of Solar Spectral Irradiance Model for Current and Future Remote Sensing Satellite Missions

Remote. Sens. Pub Date : 2023-07-03 DOI:10.3390/rs15133391
Fuqin Li, D. Jupp, B. Markham, I. Lau, C. Ong, G. Byrne, M. Thankappan, Simon Oliver, T. Malthus, P. Fearns
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Abstract

The accuracy of surface reflectance estimation for satellite sensors using radiance-based calibrations can depend significantly on the choice of solar spectral irradiance (or solar spectrum) model used for atmospheric correction. Selecting an accurate solar spectrum model is also important for radiance-based sensor calibration and estimation of atmospheric parameters from irradiance observations. Previous research showed that Landsat 8 could be used to evaluate the quality of solar spectrum models. This paper applies the analysis using five previously evaluated and three more recent solar spectrum models using both Landsat 8 (OLI) and Landsat 9 (OLI2). The study was further extended down to 10 nm resolution and a wavelength range from Ultraviolet A (UVA) to shortwave infrared (SWIR) (370–2480 nm) using inversion of field irradiance measurements. The results using OLI and OLI2 as well as the inversion of irradiance measurements were that the more recent Chance and Kurucz (SA2010), Meftah (SOLAR-ISS) and Coddington (TSIS-1) models performed better than all of the previous models. The results were illustrated by simulating dark and bright surface reflectance signatures obtained by atmospheric correction with the different solar spectrum models. The results showed that if the SA2010 model is assumed to be the “true” solar irradiance, using the TSIS-1 or the SOLAR-ISS model will not significantly change the estimated ground reflectance. The other models differ (some to a large extent) in varying wavelength areas.
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当前和未来遥感卫星任务中太阳光谱辐照度模型的选择
卫星传感器表面反射率估算的精度在很大程度上取决于用于大气校正的太阳光谱辐照度(或太阳光谱)模型的选择。选择准确的太阳光谱模型对于基于辐射度的传感器校准和根据辐照度观测估计大气参数也很重要。以前的研究表明,Landsat 8可以用来评估太阳光谱模型的质量。本文使用五个先前评估的太阳光谱模型和三个最近使用Landsat 8 (OLI)和Landsat 9 (OLI2)的太阳光谱模型进行分析。该研究进一步扩展到10纳米分辨率,波长范围从紫外线a (UVA)到短波红外(SWIR) (370-2480 nm),使用反演场辐照度测量。利用OLI和OLI2以及辐照度测量的反演结果表明,最近的Chance和Kurucz (SA2010)、Meftah (SOLAR-ISS)和Coddington (TSIS-1)模型比之前的所有模型都表现得更好。用不同的太阳光谱模型模拟大气校正得到的暗面和明面反射率特征,对结果进行了验证。结果表明,如果假设SA2010模型为“真实”太阳辐照度,使用TSIS-1或solar - iss模型不会显著改变估算的地面反射率。其他模型在不同的波长区域有所不同(有些差异很大)。
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