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Estimation of sea surface temperatures from two infrared window measurements with different absorption

McMillin, Larry M.·1975·Journal of Geophysical Research

Abstract

Radiances measured at two different wavelengths or angles, with a resulting difference in absorption, can be used to determine the atmospheric attenuation of the surface radiance so that sea surface temperatures can be derived. Previous investigations used a correction equal to a constant times the difference in measured radiances. Some of these investigations were based on radiances calculated from models that underestimated absorption in moist atmospheres. When better transmittance models were used, the accuracy decreased. Radiances at 835 cm−1 are calculated for moist atmospheres at different zenith angles to test methods used to correct infrared measurements for atmospheric attenuation. Higher-order corrections are compared to first-order corrections and are shown to result in a significant increase in accuracy, reducing the rms error by one third, from 0.6 K to 0.4 K.

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Metadata

Authors
McMillin, L. M.
Venue
Journal of Geophysical Research
Published
1975-12-20
Volume
80
Issue
36
Pages
5113-5117
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2082271913
Cited by
528
References
0
FWCI
0.00
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Estimation of sea surface temperatures from two infrared window measurements with different absorption. https://app.cochat.ai/papers/10.1029/jc080i036p05113
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McMillin, L. M. (1975). Estimation of sea surface temperatures from two infrared window measurements with different absorption. Journal of Geophysical Research. https://doi.org/10.1029/jc080i036p05113

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