Stations cotières et station hydrologique cotière d'Abidjan années 1977, 1978 et 1979
On tables 1 to 12, daily beach surface temperatures are presented. These temperatures are also ploted on figures 2 to 5 in daily values and in 7, 15, 30 days means. Salinity variations are less important than these of temperature (Fig. 6, 7). It follows that during upwelling period, variations of dynamic height anomaly are closely correlated with temperature (Fig. 6 and 8).
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| Main Author: | |
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| Format: | article biblioteca |
| Language: | French |
| Published: |
1982-06
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| Subjects: | Atmospheric Sciences, Biology, Information Management, Côte d'Ivoire, sea surface temperature variations, coastal hydrological stations, salinity, data analysis, |
| Online Access: | http://hdl.handle.net/1834/24421 |
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| Summary: | On tables 1 to 12, daily beach surface temperatures are presented. These temperatures are also ploted on figures 2 to 5 in daily values and in 7, 15, 30 days means. Salinity variations are less important than these of temperature (Fig. 6, 7). It follows that during upwelling period, variations of dynamic height anomaly are closely correlated with temperature (Fig. 6 and 8). |
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