AustralieFrV1, Main, Curation, bibRecord, 00D416

Wind-driven upwelling in Opunohu Bay, Moorea, French Polynesia

Identifieur interne : 00D416 ( Main/Curation ); précédent : 00D415; suivant : 00D417

Wind-driven upwelling in Opunohu Bay, Moorea, French Polynesia

Auteurs : Eric Wolanski [Australie, Polynésie française] ; Bruno Delesalle [France, Polynésie française]

Source :

Estuarine, Coastal and Shelf Science [ 0272-7714 ] ; 1995.

RBID : ISTEX:83BD498D60576744D383CACFF1DB9CEB636F4330

Descripteurs français

Pascal (Inist)
- Action vent, Circulation marine, Circulation verticale, Cisaillement vent, Courant dérive, Courant marin, Mer vent, Observation océanographique, Phytoplancton, Polynésie française, Salinité, Température, Upwelling, Zone côtière.
Wicri :
- geographic : Polynésie française.
- topic : Polynésie.

English descriptors

KwdEn :
- August, Coastal zone, Delesalle, Drift current, Floor slope, French Polynesia, French polynesia, Internal waves, International symposium, Local wind, Maraamu wind, Oceanic, Oceanic waters, Oceanographic survey, Outflow, Phytoplankton, Polynesia, Previous studies, Salinity, Sea circulation, Sea current, Sluggish circulation, Temperature, Upwelling, Vertical circulation, Wind driven sea, Wind effect, Wind shear, Wind speed, Wind stress, Wolanski.
Teeft :
- August, Delesalle, Floor slope, French polynesia, Internal waves, International symposium, Local wind, Maraamu wind, Oceanic, Oceanic waters, Outflow, Polynesia, Previous studies, Salinity, Sluggish circulation, Upwelling, Wind speed, Wind stress, Wolanski.

Abstract

Abstract: Opunohu Bay is a narrow, straight, 3-km long bay on the island of Moorea, French Polynesia. The bay is open to the ocean with a water depth of about 80 m at the mouth. The sea floor slope reaches one-third offshore. Field observations show that a wind blowing to offshore along the axis of the bay generates an outflow at the surface and an inflow below 20 m depth. A localized upwelling results at the mouth of the bay which may also be detected in the phytoplankton population. This situation is modelled numerically and the results suggest that the wind stress must be taken to be not only a function of the wind speed but also of the wind fetch.

Url:

https://api.istex.fr/document/83BD498D60576744D383CACFF1DB9CEB636F4330/fulltext/pdf

DOI: 10.1016/0272-7714(95)90013-6

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ISTEX:83BD498D60576744D383CACFF1DB9CEB636F4330

Le document en format XML

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<front><div type="abstract" xml:lang="en">Abstract: Opunohu Bay is a narrow, straight, 3-km long bay on the island of Moorea, French Polynesia. The bay is open to the ocean with a water depth of about 80 m at the mouth. The sea floor slope reaches one-third offshore. Field observations show that a wind blowing to offshore along the axis of the bay generates an outflow at the surface and an inflow below 20 m depth. A localized upwelling results at the mouth of the bay which may also be detected in the phytoplankton population. This situation is modelled numerically and the results suggest that the wind stress must be taken to be not only a function of the wind speed but also of the wind fetch.</div>
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Serveur d'exploration sur les relations entre la France et l'Australie

Wind-driven upwelling in Opunohu Bay, Moorea, French Polynesia

Wind-driven upwelling in Opunohu Bay, Moorea, French Polynesia

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