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Proceedings Paper

Comparison between analytical and Monte Carlo hyperspectral reflectance models for coastal remote sensing
Author(s): Charles R. Bostater Jr.; Manuel Gimond
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Paper Abstract

This paper describes an analytical 2 flow equations solution and compares it to a Monte Caro model of the photon flux in water. Both models are designed to generate synthetic water surface reflectance signatures as well as the vertical profiles of light in a homogeneous or non-homogeneous water column of specified depth and bottom reflectance. In this paper we compare and contrast the results of the models and develop a theoretically based attenuation function of both models. The results from the Monte Carlo model are used to compare a form of a 2nd order attenuation term (Psi) , resulting from a solution of the 2-flow equation, to 3 downwelling irradiance dependent terms. The results show that (Psi) differs from the three terms by 1 to 14 percent depending on the scattering to absorption ratio and volume scattering function. The result also show that (Psi) is dependent on the shape factor.

Paper Details

Date Published: 14 January 2002
PDF: 15 pages
Proc. SPIE 4544, Remote Sensing of the Ocean and Sea Ice 2001, (14 January 2002); doi: 10.1117/12.452749
Show Author Affiliations
Charles R. Bostater Jr., Florida Institute of Technology (United States)
Manuel Gimond, Florida Institute of Technology (United States)

Published in SPIE Proceedings Vol. 4544:
Remote Sensing of the Ocean and Sea Ice 2001
Charles R. Bostater Jr.; Rosalia Santoleri, Editor(s)

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