Abstract
The stationary vertical distribution of a weightless radioactive substance is considered supposing a horizontal homogeneity. A two-layer exponent law of the height is accepted for the vertical turbulent diffusion coefficient. The obtained solution is applied to the surface layer using the results ofMonin andObukhov about its structure.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Archiv für Meteorologie, Geophysik und Bioklimatologie Serie A
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
