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 |
|---|---|
| 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
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