Geofisica pura e applicata

, Volume 55, Issue 1, pp 164–174 | Cite as

The expansion of clusters of particles under the action of atmospheric macroturbulence

  • F. Mesinger
  • O. Milovanović
Article

Summary

Making use of a 500 mb numerical forecast some problems of atmospheric large-scale diffusion are investigated. The expansion of various sets of clusters of particles is compared with the predictions based on the similarity theory of homogeneous turbulence. The spreading rates were in the beginning of the period of the forecast in a good agreement with the theoretical prediction, but later on they fell to the values considerable smaller than the predicted ones. The reasons of such behaviour are discussed. Furthermore the difference in zonal and meridional expansion of the clusters is demonstrated, the zonal expansion rates being more than one order of magnitude greater than the meridional ones.

Keywords

Theoretical Prediction Spreading Rate Expansion Rate Similarity Theory Homogeneous Turbulence 
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References

  1. (1).
    Batchelor K. G.:Application of the similarity theory of turbulence to atmospheric diffusion. Quart. J. R. Meteor. Soc., 76, 133–146 (1950).Google Scholar
  2. (2).
    Djuric D.:On the accuracy of air trajectory computations. J. Meteor., 18, 597–605 (1961).Google Scholar
  3. (3).
    Durst C. S., A. F. Crossley &N. E. Davis:Horizontal diffusion in the atmosphere as determined by geostrophic trajectories. J. Fluid Mech., 6, 401–422 (1959).Google Scholar
  4. (4).
    Gifford F.:Relative atmospheric diffusion of smoke puffs. J. Meteor., 14, 410–414 (1957).Google Scholar
  5. (5).
    Gifford F.:Further data on relative atmospheric diffusion. J. Meteor., 14, 475–476 (1957).Google Scholar
  6. (6).
    Hollmann G.:Transformation der Grundgleichungen der dynamischen Meteorologie in Koordinaten der stereographischen Projektion zum Zwecke der numerischen Vorhersage. Beitr. Phys. Atmos., 31, 162–176 (1959).Google Scholar
  7. (7).
    Mesinger F.:Remarks on the behaviour of computed air trajectories near the boundaries of an octagonal area. Beitr. Phys. Atmos., 36, 21–23 (1963).Google Scholar
  8. (8).
    Pasquill F.:Atmospheric diffusion. London, Van Nostrand, 297 pp. (1962).Google Scholar
  9. (9).
    Phillips N. A.:The general circulation of the atmosphere: a numerical experiment. Quart. J. R. meteor. Soc., 82, 123–164 (1956).Google Scholar
  10. (10).
    Welander P.:Studies on the general development of motion in a two-dimensional, ideal fluid. Tellus, 7, 141–156 (1955).Google Scholar
  11. (11).
    Wippermann F., P. Gburcik &W. Klug:Zur Eulerschen und Lagrangeschen Statistik sehr grossräumiger atmosphärischer Bewegungen. Beitr. Phys. Atmos., 36, 39–69 (1963).Google Scholar

Copyright information

© Istituto Geofisico Italiano 1963

Authors and Affiliations

  • F. Mesinger
    • 1
  • O. Milovanović
    • 1
  1. 1.Department of MeteorologyUniversity of Belgrade(Yugoslavia)

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