Add to ORKGSteady-state solutions of the vertical heat-balance equation have been obtained for various assumed vertical profiles of the vertical component of velocity and eddy conductivity. Relationships have been found for the depth and the thickness of the thermocline in terms of parameters that characterize the vertical velocity and eddy conductivity. Two of the solutions agree with observations in regions having respectively divergent and convergent Ekman mass transport
We re-visit the linear model of a thermally-driven ocean in a single hemisphere, to understand depen...
Author Posting. © American Meteorological Society, 2008. This article is posted here by permission o...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
The nature of the steady buoyancy-driven circulation is investigated using multi-level numerical mod...
Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1971.Bibliography: lea...
Three new classes of exact solution of the thermocline equations are obtained through use of an ansa...
A new similarity approach is applied to the thermocline equations in order to examine contrasting fr...
The vertical flux beneath the surface boundary layer is determined by balancing the divergence induc...
A two-layer model of mid-oceanic thermocline is developed, and a comparison of the depth and tempera...
The role of baroclinic eddies in transferring thermal gradients laterally, and thus determining the ...
We offer a simple model for studying the joint effect of baroclinicity and relief (jebar) on large-s...
In this paper, we analyze one-, two- and three-dimensional numerical solutions of a simple, inertia-...
We re-visit the linear model of a thermally-driven ocean in a single hemisphere, to understand depen...
Author Posting. © American Meteorological Society, 2008. This article is posted here by permission o...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
The nature of the steady buoyancy-driven circulation is investigated using multi-level numerical mod...
Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1971.Bibliography: lea...
Three new classes of exact solution of the thermocline equations are obtained through use of an ansa...
A new similarity approach is applied to the thermocline equations in order to examine contrasting fr...
The vertical flux beneath the surface boundary layer is determined by balancing the divergence induc...
A two-layer model of mid-oceanic thermocline is developed, and a comparison of the depth and tempera...
The role of baroclinic eddies in transferring thermal gradients laterally, and thus determining the ...
We offer a simple model for studying the joint effect of baroclinicity and relief (jebar) on large-s...
In this paper, we analyze one-, two- and three-dimensional numerical solutions of a simple, inertia-...
We re-visit the linear model of a thermally-driven ocean in a single hemisphere, to understand depen...
Author Posting. © American Meteorological Society, 2008. This article is posted here by permission o...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...