Abstract
The Gulf of Fos receives part of the discharge of the Rhone river. A simple numerical model couples the physical processes of estuarine circulation, density stratification, and particulate resuspension, with the microbiological processes of light and nutrient controlled growth of pelagic micro-algae, bacteria and protozoans, and the detrital remineralisation of nutrients in water-column and sediment. Simple numerical experiments are used to show 1) the role of the Gulf in cycling land-derived nutrients before they reach the open sea; 2) the importance of particular resuspension in controlling light availability for photosynthesis and the export of organic material; and 3) the high frequency of variability in this shallow, wind-forced system. -from Authors
| Originalsprache | English |
|---|---|
| Seiten (von - bis) | 39-58 |
| Seitenumfang | 20 |
| Fachzeitschrift | Vie et Milieu |
| Jahrgang | 44 |
| Ausgabenummer | 1 |
| Publikationsstatus | Published - 1994 |
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