Titlebook: Ocean Circulation Theory; Joseph Pedlosky Book 1996 Springer-Verlag Berlin Heidelberg 1996 Equatorial Currents.Ocean.Ocean Circulation.Oce

Initiative

arcane

Buoyancy Forced Circulation and Cross-Gyre Flow,This chapter discusses two subjects which appear at first sight unconnected, but which in fact are linked by the underlying question of the way in which information is propagated in the dynamics of the ocean circulation.

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Aspirin

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細(xì)胞膜

Homogeneous Models of the Ocean Circulation,stant density) ocean if the bottom is flat, and if the bottom friction is small in the sense described in Section 1.4. Thus both a stratified and a homogeneous model would have the same Sverdrup transport for the same wind stress. This has encouraged the belief that the homogenous model, more tracta

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Vertical Structure: Baroclinic Quasi-Geostrophic Models,d, takes place in the upper 1–2 km of the ocean and then diminishes dramatically with depth. Although it is difficult to obtain reliable measurements of time-averaged velocity in the midocean because of the presence of fluctuations on time scales of months, the signature of this intensification of t

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Keratectomy

Equatorial Dynamics of the Thermocline: The Equatorial Undercurrent,es. Although the Coriolis acceleration due to the tangential component of the earth’s rotation vector remains different from 0 at the equator, for the large scales of motion under consideration in this chapter its effect is negligible. Whereas the horizontal pressure gradient outside the tropical zo

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