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| Ali, M M; Simon, B; Desai, P S. |
| Vertical motion in the equatorial Indian Ocean in the form of vertical displacements of the thermocline is studied during the Monex-79 summer monsoon season. These displacements are associated with the jet-like surface response of the equatorial ocean to zonal windstress reversal at the time of the onset of the monsoon. The surface windstress distribution and variations are obtained indirectly from GOES geosynchronous satellite low-cloud motion winds by utilizing suitable collateral data. The sea-surface-temperature field from the TIROS-N satellite is also examined. A more complete experiment involving INSAT, NOAA, microwave satellites, in situ data, numerical models and biological component is proposed (EQUINOX), signifying the response to seasonal... |
| Tipo: Text |
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| Ano: 1987 |
URL: http://archimer.ifremer.fr/doc/00267/37848/35929.pdf |
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