Abstract
Abstract The spindown of an ocean is investigated, using a two-layer numerical model. At the initial instant, a pool of warm water the size of the Coral Sea occupies the subtropical portion of the top layer; the pool is initially in geostrophic balance, with depth-averaged flow equal to zero. The ocean is allowed to develop freely in the absence of wind and heating. Horizontal temperature contrasts are very weak, so the flow is accurately linear. The warm pool first moves to the western boundary, via internal Rossby waves. A progressive wave of downwelling then develops, which transports heat up to the equator, along the equator, and around the eastern and poleward boundaries; the region of warm water generated as a result near the eastern boundary is separated from the colder ocean interior by a “front,” which spreads inward via internal Rossby waves. The net effect of all these motions is to spread the pool of warm water, which was initially concentrated in a small area, out over the rest of the ocean; ...
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