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We examine problems of steady abyssal circulation using an inviscid planetary geostrophic layered model. The model includes an active wind-driven upper layer and arbitrary topography; forcing is in th...
A simple baroclinic model of the abyssal ocean circulation is formulated in which the reversals of the meridional velocity with depth, and hence the layering of the abyss, is explained by the longitud...
Simple models are developed to describe the abyssal circulation in a circumpolar ocean driven by localized annual sources of water representing convection events. Models are based on a geostrophic red...
The classic Stommel–Arons problem is revisited in the context of a basin with a general bottom topography containing an equator. Topography is taken to be smoothly varying and, as such, there are no v...
A simple linear model of the abyssal circulation is studied in which a north-south topographic slope influences the interior and boundary-layer flow. As in an earlier study, the reversals of the merid...
A theoretical rationale is given for the simulated abyssal circulation in the North Pacific detailed in Part I. A simple theory clarifies the importance of the vertical change in area of the horizonta...
A simulation was made of the abyssal circulation in the North Pacific Ocean. The model covers the whole Pacific, has realistic coastal geometry and bottom topography, and is driven by the annual mean ...
A simple barotropic model of abyssal circulation in a circumpolar ocean basin is constructed. In the presence of a sufficiently high ridge, the classical Stommel and Arons theory applies here with ver...
The study of a simple, continuously stratified model of the abyssal ocean driven by upwelling out of the abyss into the main thermocline and by source fluid entering the basin through northern, wester...
The response of the deep ocean to periodic and steady forcing by mass sources is considered, in the presence of fluid loss, diffusion, and topography, which may or may not have regions of closed plane...
Analytical and numerical models are presented for linear quasigeostrophic buoyancy-driven flow forced bya time periodic pulsating point mass source in a continuously stratified, incompressible β-plane...

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