Titlebook: Remote Assessment of Ocean Color for Interpretation of Satellite Visible Imagery; A Review Howard R. Gordon,André Y. Morel Book 1983 Spring

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Application of the Algorithms to CZCS Imagery,effects could be removed even in a horizontally inhomogeneous atmosphere. Following this Gordon et al. (1980) applied both the atmospheric correction and in — water algorithms to imagery from the Gulf of Mexico. Figure 10 shows a subscene of CZCS imagery at 443 nm from the Gulf of Mexico before and

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Summary and Conclusions,otal seston, etc.) in surface waters through measurement of the spectral radiance L.(λ) leaving the Earth’s atmosphere. The physics of this problem is well understood. That is, the constituents influence the ocean’s optical properties (a(λ) and β(γ,λ)), and given the optical properties of the ocean

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0724-5890 kton in near-surface waters produced systematic variations in the color of the ocean which could be observed from aircraft. As a direct result of this work. NASA developed the Coastal Zone Color Scanner (CZCS). which was launched on Nimbus-G (now Nimbus-7) in October 1978. (A short description of th

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Physics of Ocean Color Remote Sensing,eries of Monte Carlo simulations (Gordon, 1976) of radiative transfer in an ocean-atmosphere system characterized by realistic and vertical distributions of all pertinent optical properties in the atmosphere, and a representative set of optical properties for the ocean (assumed homogeneous), three simplifying facts emerge.