Add to ORKGThis paper uses a theoretical model to demonstrate the existence of a group of equatorially trapped, high-frequency (wave-periods shorter than one week), meso-to-small-scale (wave-lengths shorter than 100 km), baroclinic waves which are embedded in a geostrophic current with only vertical shear. Due to their relatively large vertical and meridional velocities, these high-frequency equatorial waves may play an important role in transporting momentum as well as heat energy in the vertical and transequatorial directions
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Eart...
Thesis (Ph. D.)--University of Washington, 1988The interaction of long equatorial Rossby waves with ...
Time series of baroclinic potential energy in the upper 500 meters of the North Pacific (20-50N, 145...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
A method is developed for calculating the response of an unbounded inviscid ocean to wind stress and...
The response of the deep equatorial ocean to an oscillatory baroclinic western boundary current is i...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Evidence is presented for the generation of planetary waves by barotropic instability within the cyc...
A linear theory is presented for the flow of equatorial Kelvin waves and of the equatorial undercurr...
Standing equatorial wave modes are shown to be exact solutions of the forced, linear, inviscid shall...
A wave-induced stirring and transport mechanism for the mid-depth equatorial ocean is proposed and e...
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Eart...
Thesis (Ph. D.)--University of Washington, 1988The interaction of long equatorial Rossby waves with ...
Time series of baroclinic potential energy in the upper 500 meters of the North Pacific (20-50N, 145...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
A method is developed for calculating the response of an unbounded inviscid ocean to wind stress and...
The response of the deep equatorial ocean to an oscillatory baroclinic western boundary current is i...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Evidence is presented for the generation of planetary waves by barotropic instability within the cyc...
A linear theory is presented for the flow of equatorial Kelvin waves and of the equatorial undercurr...
Standing equatorial wave modes are shown to be exact solutions of the forced, linear, inviscid shall...
A wave-induced stirring and transport mechanism for the mid-depth equatorial ocean is proposed and e...
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Eart...
Thesis (Ph. D.)--University of Washington, 1988The interaction of long equatorial Rossby waves with ...
Time series of baroclinic potential energy in the upper 500 meters of the North Pacific (20-50N, 145...