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Atmospheric correction of satellite observations of ocean color with the Navy aerosol model

机译:海洋气溶胶模型的海洋卫星观测大气矫正

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Atmospheric correction of ocean colour is routinely achieved by fitting radiometric observations at near near-infrared wavelengths to radiances predicted for a range of aerosol types. The best-fitting candidate aerosol model can then be used to compute radiances in the visible part of the spectrum, enabling an atmospheric correction to be applied there. The Navy Aerosol Model (NAM) is a multi-component aerosol model which may be suitable for this purpose. The components of NAM are closely tied to the physical processes which generate them and this allows for some expectation on the spatial homogeneity of the component optical depths. Presented is an atmospheric correction scheme based upon NAM and implemented for SeaWiFS. Some conclusions are drawn about the efficacy of extrapolating to visible wavelengths those estimates of aerosol type and amount made at near-infrared wavelengths.
机译:通过在近红外波长的近近红外波长的辐射观察到预测一系列气溶胶类型的辐射观察,常规实现海洋颜色的大气校正。然后可以使用最合适的候选气溶胶模型来计算光谱的可见部分中的辐射,从而实现大气校正。海军气溶胶模型(NAM)是一种多分量气溶胶模型,可适用于此目的。 NAM的组件与产生它们的物理过程密切相关,这允许对部件光学深度的空间均匀性进行一些预期。呈现是基于NAM的大气修正方案,为Seawifs实施。一些结论是关于外推到可见波长的那些气溶胶类型和近红外波长的量的估计的疗效。

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