Add to ORKGThe linear stability of a one layer turbulent slab model of the mixed layer over a continuously stratified, inviscid, infinite depth ocean is investigated for large horizontal scale (≥ 0 (1 km)) perturbations…
Mutual effects of progressive wave motion in shallow water and in underlaying fluid sediments are di...
This work examines the instabilities of steady circulations driven by stationary single-gyre wind fo...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
1. Introduction The problem of the steady circulation in an inviscid, two-layer ocean is solved in ...
This paper presents a simplified model of the process through which a geostrophic flow enhances the ...
The object of this study is to explain the occurrence of relatively large amplitude inertial motion ...
Solutions are obtained for systems of equations that determine the development of velocity profiles ...
A 1-dimensional slab model is developed that describes the deepening of the well-mixed surface layer...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
A model that represents a complex local theory concerning the navifacial planetary boundary layer is...
A laboratory model is used to investigate the effects of sloping boundaries on homogeneous wind-driv...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
Reprinted from Journal of Physical Oceanography, Vol.7, No.3, May 1977.The article of record as publ...
An idealized model of the transmission of near-inertial waves from the mixed layer into the deeper o...
Mutual effects of progressive wave motion in shallow water and in underlaying fluid sediments are di...
This work examines the instabilities of steady circulations driven by stationary single-gyre wind fo...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
1. Introduction The problem of the steady circulation in an inviscid, two-layer ocean is solved in ...
This paper presents a simplified model of the process through which a geostrophic flow enhances the ...
The object of this study is to explain the occurrence of relatively large amplitude inertial motion ...
Solutions are obtained for systems of equations that determine the development of velocity profiles ...
A 1-dimensional slab model is developed that describes the deepening of the well-mixed surface layer...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
A model that represents a complex local theory concerning the navifacial planetary boundary layer is...
A laboratory model is used to investigate the effects of sloping boundaries on homogeneous wind-driv...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
Reprinted from Journal of Physical Oceanography, Vol.7, No.3, May 1977.The article of record as publ...
An idealized model of the transmission of near-inertial waves from the mixed layer into the deeper o...
Mutual effects of progressive wave motion in shallow water and in underlaying fluid sediments are di...
This work examines the instabilities of steady circulations driven by stationary single-gyre wind fo...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...