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Volumn 17, Issue 10, 1978, Pages 1631-1636

Removal of atmospheric effects from satellite imagery of the oceans

Author keywords

[No Author keywords available]

Indexed keywords

OCEANOGRAPHY; REMOTE SENSING;

EID: 0017973618     PISSN: 1559128X     EISSN: 21553165     Source Type: Journal    
DOI: 10.1364/AO.17.001631     Document Type: Article
Times cited : (305)

References (15)
  • 1
    • 84911545989 scopus 로고
    • Monitoring Coastal Water Properties and Current Circulation with ERTS-1
    • Washington, D.C. (10-14 December)
    • V. Klemas, M. Otley, and C. Wethe, "Monitoring Coastal Water Properties and Current Circulation with ERTS-1," Third ERTS-1 Symposium, Washington, D.C. (10-14 December 1973).
    • (1973) Third ERTS-1 Symposium
    • Klemas, V.1    Otley, M.2    Wethe, C.3
  • 4
    • 84957468132 scopus 로고
    • Ocean Color Analysis
    • Visibility Lab., San Diego, Calif. (April)
    • S. Q. Duntley et al., "Ocean Color Analysis," SIO Ref. 74-10, Visibility Lab., San Diego, Calif. (April 1974).
    • (1974) SIO Ref. 74-10
    • Duntley, S.Q.1
  • 7
    • 0016985086 scopus 로고
    • Placing a hypothetical Lambertian reflector of albedo A just beneath the sea surface results in nearly the same computed upward radiance at the top of the atmosphere as that obtained in complete simulations of radiative transfer in the ocean-atmosphere system as long as A = R. r in Eq. (1) is the ratio of the number of photons which interact twice with this Lambertian surface to the number which interact once
    • H. R. Gordon, Appl. Opt. 15, 1974 (1976). Placing a hypothetical Lambertian reflector of albedo A just beneath the sea surface results in nearly the same computed upward radiance at the top of the atmosphere as that obtained in complete simulations of radiative transfer in the ocean-atmosphere system as long as A = R. r in Eq. (1) is the ratio of the number of photons which interact twice with this Lambertian surface to the number which interact once.
    • (1976) Appl. Opt , vol.15 , pp. 1974
    • Gordon, H.R.1
  • 8
    • 84975639120 scopus 로고    scopus 로고
    • 1(0, ϕ) is removed from I(0, ϕ), one is still faced with the fact that the photons leaving the ocean have to pass through the atmosphere, reducing the contrast with which horizontal variations in R (and hence ocean properties) can be observed. This imaging aspect of the problem will be dealt with in a later paper
    • 1(0, ϕ) is removed from I(0, ϕ), one is still faced with the fact that the photons leaving the ocean have to pass through the atmosphere, reducing the contrast with which horizontal variations in R (and hence ocean properties) can be observed. This imaging aspect of the problem will be dealt with in a later paper.
  • 13
    • 77957076640 scopus 로고
    • Scattered Radiation in the Atmosphere and the Natural Aerosol
    • (Academic P., New York)
    • K. Bullrich, Scattered Radiation in the Atmosphere and the Natural Aerosol, in Advances in Geophysics (Academic P., New York, 1964), Vol. 10.
    • (1964) Advances in Geophysics , vol.10
    • Bullrich, K.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.