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首页> 外文期刊>Applied optics >Uncertainty in global downwelling plane irradiance estimates from sintered polytetrafluoroethylene plaque radiance measurements
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Uncertainty in global downwelling plane irradiance estimates from sintered polytetrafluoroethylene plaque radiance measurements

机译:烧结聚四氟乙烯斑块辐射测量的全球贫困平面辐照度的不确定性

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摘要

Global downwelling plane irradiance is a necessary variable to normalize water-leaving radiance measurements, reducing the magnitude and spectral variabilities introduced by the incident light field. As a result, the normalized measurements, known as remote sensing reflectance, have higher correlation with the inherent optical properties of the water body and so to the composition of optically active water components. For in situ measurements, the global downwelling plane irradiance can be estimated from the exitant radiance of sintered polytetrafluoroethylene plaques or other diffuse reflectance standards. This allows use of a single spectrometer to measure all necessary variables to estimate the remote sensing reflectance, reducing cost in acquisition and maintenance of instrumentation. However, despite being in use for more than 30 years, the uncertainty associated with the method has been only partially evaluated. In this study, we use a suite of sky radiance distributions for 24 atmospheres and nine solar zenith angles in combination with full bidirectional reflectance distribution function determinations of white and gray plaques to evaluate the uncertainties. The isolated and interactive effects of bidirectional reflectance distribution, shadowing, and tilt error sources are evaluated. We find that under the best-performing geometries of each plaque, and with appropriate estimation functions, average standard uncertainty ranges from 1% to 6.5%. The simulated errors are found to explain both previous empirical uncertainty estimates and new data collected during this study. Those errors are of the same magnitude as uncertainties of plane irradiance sensors (e. g., cosine collectors) and overlap with uncertainty requirements for different uses of in situ data, which supports the continued use of the plaque method in hydrologic optics research and monitoring. Recommendations are provided to improve the quality of measurements and assure that uncertainties will be in the range of those calculated here. (c) 2019 Optical Society of America.
机译:全球贫困平面辐照度是一个必要的变量,以归一化水留辐射测量,从而降低入射光场引入的幅度和光谱变化。结果,称为遥感反射率的归一化测量与水体的固有光学性质等更高的相关性,以及光学活性水组成的组成。对于原位测量,可以从烧结的聚四氟乙烯斑块或其他漫射反射标准的出口辐射估计全球贫寒平面辐照度。这允许使用单光谱仪来测量所有必要的变量来估计遥感反射率,降低获取和维护仪器的成本。然而,尽管使用了30多年来,但仅部分评估了与该方法相关的不确定性。在这项研究中,我们使用一套天空辐射分布,用于24个大气和九个太阳能天性角度,结合全双向反射率分布函数确定白色和灰色斑块来评估不确定性。评估双向反射分布,阴影和倾斜误差源的隔离和交互式效果。我们发现,在每个牙菌斑的最佳性几何形状下,具有适当的估计功能,平均标准不确定性范围为1%至6.5%。发现模拟错误来解释本研究期间收集的以前的经验不确定性估计和新数据。这些误差与平面辐照度传感器的不确定性相同(例如,余弦收集器)并与原位数据的不同用途的不确定性要求重叠,这支持在水文学光学研究和监测中继续使用斑块方法。提供了建议,以提高测量质量,并确保不确定性将在此计算的范围内。 (c)2019年光学学会。

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