Abstract
The operation characteristics of a rotating hydraulic channel, designed for geophysical fluid-dynamic research, are described. The results of simulations concerning the conditions of motion and density stratification of the atmospheric planetary boundary layer, both stationary and in evolution, are then presented.
Original language | English |
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Pages (from-to) | 427-438 |
Number of pages | 12 |
Journal | Nuovo Cimento della Societa Italiana di Fisica C |
Volume | 12 |
Issue number | 4 |
DOIs | |
Publication status | Published - Jul 1989 |
Externally published | Yes |
Keywords
- Meteorology