Abstract
IN 1912–13, F. E. Fowle1 made studies of the absorption of infra-red radiation by water-vapour at 0.93μ, 1.13μ and 1.47μ, in order to determine spectroscopically the total water-vapour content of the atmosphere. The first two wave-lengths are at the centres of the ρ and ϕ bands; the last is about 450 cm.−1 from the Ψ-band centre.
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References
Fowle, F. E., Astrophys. J., 35, 149 (1912); 37, 359 (1913).
Mecke, R., Z. Phys., 81, 313 (1933).
Nielsen, H. H., Phys. Rev., 59, 565 (1941); 62, 422 (1942).
Randall, H. M., Dennison, D. M., Ginsburg, N., and Weber, L. R., Phys. Rev., 52, 160 (1937).
Abbott, C. G., and Freeman, H. B., Smithson. Misc. Coll., 82, No. 1 (1929).
Langley, S. P., Ann. Astrophys. Obs., 1, table 23 (1900).
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COWLING, T. Hitherto Unidentified Absorption Bands of Water Vapour. Nature 152, 694 (1943). https://doi.org/10.1038/152694a0
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DOI: https://doi.org/10.1038/152694a0