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Applied Optics

Applied Optics

APPLICATIONS-CENTERED RESEARCH IN OPTICS

  • Vol. 14, Iss. 2 — Feb. 1, 1975
  • pp: 417–427

Computed Relationships Between the Inherent and Apparent Optical Properties of a Flat Homogeneous Ocean

Howard R. Gordon, Otis B. Brown, and Michael M. Jacobs  »View Author Affiliations


Applied Optics, Vol. 14, Issue 2, pp. 417-427 (1975)
http://dx.doi.org/10.1364/AO.14.000417


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Abstract

Monte Carlo simulations of the transfer of radiation in the ocean are used to compute the apparent optical properties of a flat homogeneous ocean as a function of the inherent optical properties. The data are used to find general relationships between the inherent and apparent optical properties for optical depths τ ≤ 4. The results indicate that the apparent optical properties depend on the phase function only through the back scattering probability. It is shown that these relations can be used with measurements of the upwelling and downwelling irradiance, the beam attenuation coefficient, and the incident radiance distribution to determine the absorption coefficient, the scattering coefficient, and the backward and forward scattering probabilities.

© 1975 Optical Society of America

History
Original Manuscript: July 19, 1974
Published: February 1, 1975

Citation
Howard R. Gordon, Otis B. Brown, and Michael M. Jacobs, "Computed Relationships Between the Inherent and Apparent Optical Properties of a Flat Homogeneous Ocean," Appl. Opt. 14, 417-427 (1975)
http://www.opticsinfobase.org/ao/abstract.cfm?URI=ao-14-2-417


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References

  1. T. J. Petzold, Volume Scattering Functions for Selected Waters (Scripps Institution of Oceanography, University of California at San Diego, 1972), SIO Ref. 72–78.
  2. N. G. Jerlov, Optical Oceanography (Elsevier, Amsterdam, 1968).
  3. J. E. Tyler, R. C. Smith, Measurements of Spectral Irradiance Underwater (Gordon and Breach, New York, 1970).
  4. R. W. Preisendorfer, U.G.G.I., Monogr. 10, 11 (1961).
  5. J. E. Tyler, R. C. Smith, W. H. Wilson, J. Opt. Soc. Am. 62, 83 (1972). [CrossRef]
  6. H. R. Gordon, Appl. Opt. 12, 2803 (1973). [CrossRef] [PubMed]
  7. In this work μ is always cosθ, and unprimed μ’s refer to rays beneath the sea surface, while primed μ’s refer to rays above the sea surface.
  8. H. R. Gordon, O. B. Brown, Appl. Opt. 12, 1544 (1973). [CrossRef]
  9. G. Kullenberg, Deep Sea Res. 15, 423 (1968).
  10. G. N. Plass, G. W. Kattawar, J. Binstock, J. Quant. Spectrosc. Radiat. Transfer. 13, 1081 (1973). [CrossRef]
  11. G. N. Plass, G. W. Kattawar, F. E. Catchings, Appl. Opt. 12, 314 (1973). [CrossRef] [PubMed]
  12. L. Prieur, A. Morel, Cahiers Ocean 23, 35 (1971).
  13. G. F. Beardsley, J. R. V. Zaneveld, J. Opt. Soc. Am. 59, 373 (1969). [CrossRef]
  14. C. Cox, W. Munk, J. Opt. Soc. Am. 44, 838 (1954). [CrossRef]
  15. G. Maul, H. R. Gordon. Relationships Between ERTS Radiances and Gradients across Oceanic Fronts, presented at the Third ERTS-1 Principal Investigator’s Symposium.
  16. H. R. Gordon, W. R. McCluney, Appl. Opt. 14, 413 (1975). [CrossRef] [PubMed]
  17. M. Herman, J. Lenoble, J. Quant. Spectrosc. Radiat. Transfer 8, 355 (1968).

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