Summary
The measurement of condensation nucleus concentration from an aircraft is considered and preliminary observations made with a photo-electric condensation nucleus counter discussed. It is concluded that at heights up to 6000 ft concentrations of condensation nuclei vary, from 200 cm−3 in clean maritime air to 5 × 103 cm−3 generally over large industrial areas and 35 × 103 cm−3 downwind of specific industrial sources. It appears that sea spray makes a contribution to the nucleus population.
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References
Pollak L. W. & Murphy T., Archiv für Meteorologie, Geophysik und Bioklimatologie, Serie A, p. 101 (1953).
Dessens H., La Meteor, pp. 321–327, 328–340 (1947).
Wigand A., Ann. der Physik., 59, 689–742 (1919).
Pollak L. W., Geofisica pura e applicata, Vol. 22 (1952).
Junge C., Compendium of Meteorology, p. 186 (1951).
Simpson, Quart. Journ. R. Met. Soc., 67 99 (1941).
Additional information
Mr. G. J.Day, B. Sc., Meteorological Research Flight, Royal Aircraft Establishment,Farnborough, Hants. (Great Britain).
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Day, G.J. Some airborne observations of condensation nucleus concentration. Geofisica Pura e Applicata 31, 169–181 (1955). https://doi.org/10.1007/BF01999599
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DOI: https://doi.org/10.1007/BF01999599