Add to ORKGUnder usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the equator and a maximum one west of 170E. After the appearance of EI Nino, this maximum is replaced by another one located in the Central South Pacific; this feature has been observed in 1972-73 but also in 1957-58 and 1976-77. The mechanism involves probable change of the mixed layer depth
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
Thesis (Ph.D.)--University of Washington, 2018The oceanic surface mixed layer (ML) heat and salinity...
This paper presents the results of an experiment in the western equatorial Pacific centered on the e...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over tw...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
All available navifacial data from 1956 to 1974 have been compiled to produce two charts per year of...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
Thesis (Ph.D.)--University of Washington, 2018The oceanic surface mixed layer (ML) heat and salinity...
This paper presents the results of an experiment in the western equatorial Pacific centered on the e...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over tw...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
All available navifacial data from 1956 to 1974 have been compiled to produce two charts per year of...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
Thesis (Ph.D.)--University of Washington, 2018The oceanic surface mixed layer (ML) heat and salinity...