Add to ORKGDescribed in this paper is a technique of using artificial water boundaries in theories of ocean currents. As boundary values, geostrophic currents are suggested. This technique may hold promise for other applications in theoretical discussions of ocean currents
Quantitative agreement between geostrophic computations and direct measurements of current and trans...
An important dynamical question involves how oceanic balanced flows lose energy. Recent numerical an...
An inertial multi-layer model of the recirculation gyres surrounding a separated boundary current is...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
1. Introduction The problem of the steady circulation in an inviscid, two-layer ocean is solved in ...
The linear equations governing stratified, wind-driven flow in an ocean of arbitrary shape may be co...
The simplest problem in the formation of an inertial stratified western-boundary current on a contin...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1974.Vita.Bibliography...
When a current is crossed by a vessel on fixed course at fixed speed, the vessel is displaced downst...
The generation of longshore currents on a beach is investigated theoretically, using the concept of ...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
The question of the dynamics of the equatorial counter currents of the several oceans was scarcely b...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Quantitative agreement between geostrophic computations and direct measurements of current and trans...
An important dynamical question involves how oceanic balanced flows lose energy. Recent numerical an...
An inertial multi-layer model of the recirculation gyres surrounding a separated boundary current is...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
1. Introduction The problem of the steady circulation in an inviscid, two-layer ocean is solved in ...
The linear equations governing stratified, wind-driven flow in an ocean of arbitrary shape may be co...
The simplest problem in the formation of an inertial stratified western-boundary current on a contin...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1974.Vita.Bibliography...
When a current is crossed by a vessel on fixed course at fixed speed, the vessel is displaced downst...
The generation of longshore currents on a beach is investigated theoretically, using the concept of ...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
The question of the dynamics of the equatorial counter currents of the several oceans was scarcely b...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Quantitative agreement between geostrophic computations and direct measurements of current and trans...
An important dynamical question involves how oceanic balanced flows lose energy. Recent numerical an...
An inertial multi-layer model of the recirculation gyres surrounding a separated boundary current is...