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• W2026696311 abstract "The hydrography, wind, Argos and Argo measurements in the areas surrounding Luzon Strait were collected. Based on the hydrographic data obtained during September 1994, the improved Princeton Ocean Model using a generalized topography-following coordinate system together with a modified inverse method was applied to study the circulation in September. Observations and the diagnostic simulation produce a consistent circulation pattern, and the main dynamical features can be summarized as follows. (1) The Kuroshio has two branches with the main Kuroshio existing above 800 m depth and the western part existing above 400 m depth. The western branch of the Kuroshio leaves the main current near 20.5°N, then flows northwestward through Luzon Strait and finally flows out of the northern boundary southwest of Taiwan, consistent with the trajectory of Argos drifters. (2) The non-linear term is important and cannot be neglected in the momentum equations in the northern part of Luzon Strait under the baroclinicity field. Using non-linear dynamics, the westward intrusion of the Kuroshio into the northern part of Luzon Strait is more curved than when using linear dynamics. However, the non-linear term is smaller and so negligible around Luzon Strait under the homogeneous density field. (3) In the area from 117°E to 119°E and from 20.2°N to 21.7°N, an anticyclonic eddy appears east of Dongsha Islands. (4) At depths above 400 m, the circulation is mainly dominated by the basin-scale cyclonic gyre. (5) In the computational domain west of 121°E, the circulation below 800 m is mainly dominated by the basin-scale anticyclonic gyre. (6) The South China Sea water flows eastward across Luzon Strait in the middle layers, then turns cyclonically, finally flowing northward into the region east of Taiwan Island, which is qualitatively in agreement with the trajectories of Argo floats at about 1000 m depth in the area east of 121°E. RESUME (Traduit par la redaction) Nous avons rassemble l'hydrographie, le vent, les Argo et les mesures Argo dans les regions avoisinant le detroit de Lucon. Sur la base des donnees hydrographiques relevees durant le mois de septembre 1994, nous avons applique le modele oceanique ameliore de Princeton utilisant un systeme de coordonnees « suivant le terrain » generalise de pair avec une methode inverse modifiee pour etudier la circulation en septembre. Les observations et la simulation diagnostique produisent une configuration de circulation coherente dont on peut resumer comme suit les principales caracteristiques dynamiques. (1) Le Kuroshio possede deux branches : le Kuroshio principal existant au-dessus d'une profondeur de 800 m et la partie ouest existant au-dessus d'une profondeur de 400 m. La branche ouest du Kuroshio quitte le courant principal aux environs de 20,5°N et se dirige vers le nord-ouest a travers le detroit de Lucon pour finalement franchir la limite nord du detroit au sud-ouest de Taiwan, ce qui correspond a la trajectoire des bouees derivantes Argos. (2) Le terme non lineaire dans les equations est important et ne peut pas etre considere negligeable de quantite de mouvement dans la partie nord du detroit de Lucon dans le champ de baroclinite. Lorsqu'on utilise la dynamique non lineaire, l'intrusion vers l'ouest du Kuroshio dans la partie nord du detroit de Lucon est plus incurvee que lorsqu'on utilise la dynamique lineaire. Cependant, le terme non lineaire est plus petit et donc negligeable autour du detroit de Lucon dans le champ de densite homogene. (3) Dans la region allant de 117° E a 119°E et de 20,2°N a 21,7°N, un remous anticyclonique apparait a l'est des iles Dongsha. (4) Aux profondeurs inferieures a 400 m, la circulation est principalement dominee par le gyre cyclonique a l'echelle du bassin. (5) Dans le domaine de calcul a l'ouest de 121°E, la circulation sous 800 m est principalement dominee par le gyre anticyclonique a l'echelle du bassin. (6) Les eaux de la mer de Chine meridionale s'ecoulent vers l'est a travers le detroit de Lucon dans les couches intermediaires, puis tournent de facon cyclonique pour finalement s'ecouler vers le nord dans la region a l'est de l'ile Taiwan, ce qui, qualitativement, s'accorde avec la trajectoire des flotteurs Argo a environ 1000 m de profondeur dans la region a l'est de 121°E." @default.
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• W2026696311 date "2012-11-12" @default.
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• W2026696311 title "Circulation Around Luzon Strait in September as Inferred from CTD, Argos and Argo Measurements and a Generalized Topography-Following Ocean Model" @default.
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