Skip to main content
Log in

Equation de transport et de diffusion pour l'atmosphère turbulente avec des masses d'air différemment échauffées

  • Published:
pure and applied geophysics Aims and scope Submit manuscript

Summary

Generalization of the diffusion and transport equation are given. They refer to an atmosphere in which in addition to irregular turbulent motion exists also regular motion of the heated and cooled air masses. The equations are briefly discussed.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

Bibliographie

  1. V. Bjerknes, J. Bjerknes, H. Solberg etT. Bergeron,Physikalische Hydrodynamik mit Anwendung auf die dynamische Meteorologie (Verlag J. Springer, Berlin 1933), 693.

    Google Scholar 

  2. M. Čadež,Über den Einfluss des fallenden Schnees auf die Temperatur der trockenen Atmosphäre, Meteor. Z.56 (1939), 272.

    Google Scholar 

  3. H. L. Kuo,Further studies of the properties of collular convection in a conditionally unstable atmosphere, Tellus17 (1965), 413.

    Google Scholar 

  4. M. Čadež,Strahlstrom und der durch Turbulenz verursachte Transport der mechanischen Energie in der Atmosphäre, Geofis. pura e appl.46 (1960), 173.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Čadež, M. Equation de transport et de diffusion pour l'atmosphère turbulente avec des masses d'air différemment échauffées. PAGEOPH 64, 173–177 (1966). https://doi.org/10.1007/BF00875543

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00875543

Navigation