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Squires, P. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Observations on the droplet spectra of different kinds of warm clouds have shown that systematic differences in microstructure exist between the various cloud types. These differences in microstructure are related in a simple way to differences in observed colloidal stability.DOI: 10.1111/j.2153-3490.1958.tb02011.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • ALPERT, L., 1955: Notes on warm rainfall. Bull. Amer. Meteor. Soc., 36, NO.2, 64-68.
    • BRAHAM, R. R., S. E. RBYNOLDS, and J. H. HARRBLL, 1951: Possibilities of cloud seeding as determined by a study of cloud height versus precipitation]. Meteor., 8, 416-418.
    • BYERS, H. R., and R. K. HALL, 1955: A census of cumuluscloud height versus precipitation in the vicinity of Puerto Rico, Winter-Spring 1953-54. ]. Meteor., ra, 176-178.
    • BYBRS, H. R., 1956: Cloud Physics Research-Final report under contract No. AF 19 (604)-618, University of Chicago, January 31, 1956.
    • PBARCBY, T., and G. W. HILL, 1957: A theoretical estimate of the collection efficiencies of small droplets. Quart.]. R. Meteor Soc., 83, 77-92.
    • SQUIRES, P., and C. A. GILLBSPIB, 1952: A cloud droplet sampler for use on aircraft. Quart. J. R. Meteor Soc. '78, No. 337, 387-393.
    • SQUIRilS, P., and J. WARNER: Some observations in the orographic cloud of the Island of Hawaii and in trade-wind cumuli. Tellus, 9, 475-494.
    • SQUIRBS, P., (1956): The microstructure of cumuli in maritime and contitental air. Tellus, 8, 443:-444.
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