Ocean Circulation Theory

1. Auflage Corr. 2. printing. Softcover version of original hardcover Auflage 1996
ISBN: 978-3-642-08224-5
Verlag: Springer

Buch, Englisch, 456 Seiten, Previously published in hardcover, Format (B × H): 155 mm x 235 mm, Gewicht: 789 g

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.

Zielgruppe

Professional/practitioner

Autoren/Hrsg.

Pedlosky, Joseph

Fachgebiete

• Geowissenschaften Geologie Geodäsie, Kartographie, Fernerkundung
• Geowissenschaften Geologie Geologie
• Geowissenschaften Geologie Marine Geologie, Ozeanographie (Meereskunde)
• Geowissenschaften Geologie Aeronomie, Ionosphäre, Magnetosphäre
• Geowissenschaften Geographie | Raumplanung Geodäsie, Kartographie, GIS, Fernerkundung
• Naturwissenschaften Physik Angewandte Physik Geophysik
• Geowissenschaften Geologie Meteorologie, Klimatologie
• Geowissenschaften Geologie Geophysik

Inhaltsverzeichnis

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.