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A. Adel, C. Lampland (1940)
Atmospheric Absorption of Infrared Solar Radiation at the Lowell Observatory. III and IV. The Spectral Intervals: 8.0-11.0 μ and 11.0-14.0 μ.The Astrophysical Journal, 91
T. Cowling (1942)
The absorption of water vapour in the far infra-redReports on Progress in Physics, 9
G. Dobson, A. Brewer, B. Cwilong (1946)
Bakerian Lecture: Meteorology of the lower stratosphereProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 185
An account is given of further measurements of atmospheric radiation which confirm former conclusions regarding the errors of two types of radiation chart when used to compute total radiation at the surface. The greater part of the difference between computed and observed radiation is attributed to two causes – emission from particulate matter and the variation of emissivity of water vapour with temperature. The results suggest a form for this variation between −5°C and +25°C.
The Quarterly Journal of the Royal Meteorological Society – Wiley
Published: Jan 1, 1950
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