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Original Articles

The Influence of Cloud Nucleus Population on the Microstructure and Stability of Convective Clouds

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Pages 408-411 | Received 06 Apr 1959, Published online: 15 Dec 2016

References

  • BATTAN, L. J., and REITAN, C. H., 1957: Droplet size measurements in convective clouds. Artificial Stimu-lation of Rain, Pergamon Press, pp. 184–191.
  • SQUIRES, P., 1952. The growth of cloud drops by conden-sation, Part II: the formation of large cloud drops. Aust. J. Sci. Res. A 5 (3) PP. 473-499
  • SQUIRES, P., and GILLESPIE, C. A., 1952: A cloud droplet sampler for use on aircraft. Q. J. R. M. S. 78 (337) PP- 387–393.
  • SQUIRES, P., 1956: The microstructure of cumuli in maritime and continental air. Tellus 8 pp. 443–444.
  • SQUIRES, P., 1958 a: The microstructure and colloidal stability of warm clouds, Part I: The relation between struc-ture and stability. Tellus 10 pp. 256–261.
  • SQUIRES, P., 1958 b: The microstructure and colloidal stability of warm clouds, Part II: The causes of the variations in microstructure. Tellus It), pp. 262–271.
  • SQUIRES, P., AND TWOMEY, S., 1958: Some observations relating to the stability of warm cumuli. Tellus 10, PP–272–274.
  • TWOMEY, S., 1959 a: The nuclei of natural cloud for-mation, Part I: The chemical diffusion method and its application to atmospheric nuclei. Geofisica pura e applicata, 43, pp. 227–242.
  • TWOMEY, S., 1959 b: The nuclei of natural cloud formation, Part II: The supersaturation in natural clouds and the variation of cloud droplet concentration. Geofisica pura e applicata, 43, pp. 243–249.
  • WIELAND, W., 1956: Die Wasserdampfkondensation an naturlichem Aerosol bei geringen Ubersattigungen. E. T. H. Zurich, Promotionsarbeit Nr. 2577.