Abstract
The spectral calculations of the flow which develops near a heated vertical wall in a fluid stably stratified by a salinity gradient are carried out. The case of weak stratification and heating due to a constant heat flux is considered. The numerical results are compared to the experimental ones. Both on qualitative and quantitative arguments, a satisfactory agreement is obtained. The cell formation process is discussed by focusing on the occurrence of counter-rotative cells and on the instability phenomenon of the simultaneous creation of cells. The high sensitivity of such phenomena to slight disturbances at the initial time is pointed out.
| Original language | English |
|---|---|
| Pages (from-to) | 2681-2697 |
| Number of pages | 17 |
| Journal | International Journal of Heat and Mass Transfer |
| Volume | 44 |
| Issue number | 14 |
| DOIs | |
| Publication status | Published - 5 Jun 2001 |
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