A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allows a more detailed description of the abyssal flow than has been possible before. In addition to the generally northward flow of the Pacific Bottom Water, some evidence is presented for the manner of modification of the Bottom Water, by vertical mixing and geothermal heating, into Pacific Deep Water, which must return southward above the Bottom Water layer...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
Terrestrial heat flow through the ocean floor is determined by measuring the temperature gradient an...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Values of potential temperature, salinity, and dissolved oxygen at deep levels in the central North ...
Maps of the anomaly of the geopotential distance between various deep isobaric surfaces in the Pacif...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
Terrestrial heat flow through the ocean floor is determined by measuring the temperature gradient an...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Values of potential temperature, salinity, and dissolved oxygen at deep levels in the central North ...
Maps of the anomaly of the geopotential distance between various deep isobaric surfaces in the Pacif...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
This paper presents a theoretical study of the steady-state density, pressure, and velocity fields i...
Terrestrial heat flow through the ocean floor is determined by measuring the temperature gradient an...