Ocean circulation theory [Libro electrónico] / autor: Joseph Pedlosky
Por: Pedlosky, Joseph [autor/a].
Tipo de material: Libro en línea Editor: New York, New York, United State: Springer, c1996Descripción: xi, 453 páginas : ilustraciones ; 25 centímetros.ISBN: 3540604898; 9783642082245 (Print); 9783662032046 (Online).Tema(s): Ocean circulationNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 451-453 Número de sistema: 56427Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
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Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400564274093 |
Incluye bibliografía e índice: páginas 451-453
1. Sverdrup theory.. 2. Homogeneous models of the ocean circulation.. 3. Vertical structure: baroclinic quasi-geostrophic models.. 4. Theory of the ventilated thermocline.. 5. Buoyancy forced circulation and cross-gyre flow.. 6. Equatorial dynamics of the thermocline: the equatorial undercurrent.. 7. Abyssal circulation.. Subject Index
Disponible para usuarios de ECOSUR con su clave de acceso
The waters of the earth are gathered in shallow, irregular, interconnecting basins. Heated by the sun and driven by the wind, the oceans circulate endlessly. The general circulation of the ocean is the persistent pattern of this flow on the scale of the basins. It is the heart and soul of physical oceanography, and the explanation and prediction of the flow from the principles of fluid dynamics is the chief goal of the physical oceanographer. Along with the pattern of the motion, the associated fields of pressure, temperature, salinity, and density are also necessary components of a complete theory for the ocean circulation since they are dynamically linked to the motion of the oceans. The physical problem posed by the general circulation of the oceans is a difficult one both experimentally and theoretically. From the point of view of theoretical fluid mechanics the difficulty springs fundamentally from the recirculating character of the circulation. The fluid is gathered into a single, though highly contorted basin. eng
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