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Original Articles

The Formation of Rain by Coalescence in Very Shallow Cumulus

Pages 216-219 | Received 26 Jul 1958, Published online: 15 Dec 2016

References

  • BYERS, H. R. and HALL, R. K., 1955: A census of cumulus-cloud height versus precipitation in the vicinity of Puerto Rico during the winter and spring of 1953-4. J. Met. 12, p. 176.
  • HOCKING, L. M., 1959. The collision efficiency of small drops. Quart J. Roy. Met. Soc. 85, p. 44.
  • LUDLAM, F. H. and SAUNDERS, P. M., 1956: Shower formation in large cumulus. Tellus 8, p. 424.
  • MASON, B. J., 1952: The production of rain and drizzle by coalescence in stratiform clouds. Quart. J. Roy. Met. Soc. 78, p. 377.
  • MASON, B. J. and GHosx, D. K., 1957: The formation of large droplets in small cumulus. Quart. J. Roy. Met. Soc. 83, p. 501.
  • Tellus XI (1959), 2
  • PEARCY, T. and HILL, G. W., 1957: A theoretical esti-mate of the collection efficiencies of small droplets. Quart. J. Roy. Met. Soc. 83, p. 77.
  • SQUIRES, P., 1958: The microstructure and colloidal stability of warm clouds. Tellus ID, p. 256, 262.
  • SQUIRES, P. and WARNER, J., 1957: Some measurements in the orographic cloud of the island of Hawaii and in trade wind cumuli. Tellus, 9, p. 475.
  • WOONCOCIT, A. H., 1953: Salt nuclei in marine air as a function of altitude and wind force. J. Met. Ico p. 362.
  • WOONCOCIT, A. H., 1957: The Artificial Production of Rain. Pergamon Press, London, 202 pp.