Abstract
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.
Original language | English |
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Pages (from-to) | 117-128 |
Number of pages | 12 |
Journal | Boundary-Layer Meteorology |
Volume | 62 |
Issue number | 1-4 |
DOIs | |
State | Published - 1 Jan 1993 |
ASJC Scopus subject areas
- Atmospheric Science