Possibilities of laboratory simulation of two different atmospheric layers - stratospheric and boundary layer - are considered. The laboratory simulation is performed by fully developed turbulent flows of mercury (Re∼7×104) in strong magnetic fields. The processes of direct and inverse transfer of energy and passive scalar are investigated.
|Number of pages||12|
|State||Published - 1 Jan 1993|
ASJC Scopus subject areas
- Atmospheric Science