Abstract
Atmospheric effects upon the radiometric determination of surface temperature were studied for channels centered at 3.7, 11 and 12 Μm. The error due to the atmosphere is least for the channel centered at 3.7 Μm, which is a real advantage. The use of a linear combination of two or all three of these channels allows one to eliminate most of the atmospheric effect. If instrumental noise of from 0.1 to 0.2 K is accounted for in each channel, the best results are obtained by a combination of the two channels at 3.7 and 12 Μm.
Similar content being viewed by others
References
Anding, D. and Kauth, R.: 1970, ‘Estimation of Sea Surface Temperature from Space’, Remote Sensing Environ., 1, 217–220.
Bignell, K. J.: 1970, ‘The Water Vapor Infrared Continuum’, Quart. J. Roy. Meteorol. Soc., 96, 390–403.
Brower, R. L., Gohrband, H. S., Pichel, W. G., Signore, T. L., and Walton, C. C.: 1976, ‘Satellite Derived Sea Surface Temperatures from NOAA Spacecraft’, NOAA Techn. Memorandum NESS 78.
Burch, D. E., and Gryvnak, D. A.: 1970, ‘Atmospheric Attenuation in the Infrared Windows’, in Space-Opt. Semin.-in-Depth, Santa Barbara, Calif., 1969, 17–22.
Cogan, J. L., and Willand, J. H.: 1976, ‘Measurement of Sea Surface Temperature by the NOAA 2 Satellite’, J. Appl. Meteorol. 15, 173–180.
Deschamps, P. Y.: 1977, ‘Télédétection de la température de surfaee de la mer par radiométrie infrarouge’, Thèse de Doctorat d'Etat, Université de Lille, No. 376.
Deschamps, P. Y., and Phulpin, T.: 1978, ‘Elimination de l'effet de l'atmosphère et optimisation des bandes spectrales d'un radiomètre infrarouge à un ou deux canaux pour la mesure de la température de surface des sols’, in Proc. Int. Conf. on Earth Observation from Space, Toulouse, 1978, ESA SP-134, 347–353.
Maul, G. A., and Sidran, M.: 1973, ‘Atmospheric Effects on Ocean Surface Temperature Sensing from the NOAA Satellite Scanning Radiometer’, J. Geophys. Res., 78, 1909–1916.
Meyer, W. D.: 1973, ‘Data Acquisition and Processing Program: a Meteorological Data Source’, Bull. Amer. Meteorol. Soc., 54, 1251–1254.
McMillin, L. M.: 1975, ‘Estimation of Sea Surface Temperatures from Two Infrared Window Measurements with Different Absorption’, J. Geophys. Res., 80, 5113–5117.
Pontier, L., and Dechambenoy, C.: 1966, ‘Détermination des constantes optiques de l'eau liquide entre 1 et 40 Μm’, Ann. Geophys., 22, 633–641.
Prabhakara, C., Dalu, G. and Kunde, V. G.: 1974, ‘Estimation of Sea Surface Temperature from Remote Sensing in the 11- to 13-Μm Window Region’, J. Geophys. Res., 79, 5039–5044.
Selby, J. E. A., Shettle, E. P., and McClatchey, R. A.: dy1976, ‘Atmospheric transmittance from 0.25 to 28.5 Μm: Supplement LOWTRAN 3B (1976)’, AFGL Rep. AFGL-TR-76-0258.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Deschamps, P.Y., Phulpin, T. Atmospheric correction of infrared measurements of sea surface temperature using channels at 3.7, 11 and 12 Μm. Boundary-Layer Meteorol 18, 131–143 (1980). https://doi.org/10.1007/BF00121320
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF00121320