Add to ORKGIn the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of the baroclinic gyre systems in the region from 0-400 m depth has been mapped on a yearly basis from 1954-1974. From this measure of the baroclinic field of mass, the dynamic height (0/400 db) has been computed for each year, yielding geostrophic current indices of the major zonal currents...
An array of 15 moorings with 33 current meters was deployed in the deep water across the Continental...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
Monthly mean values of temperature from both hydrographic and XBT casts are used to compute isotherm...
A time sequence of meridional baroclinic transport (0/1000 db) across the Subtropical gyre of the No...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Two data sets are used to reveal the quasi-stationary nature of the banded current structure in the ...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
Time series of baroclinic potential energy in the upper 500 meters of the North Pacific (20-50N, 145...
An array of 15 moorings with 33 current meters was deployed in the deep water across the Continental...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
Monthly mean values of temperature from both hydrographic and XBT casts are used to compute isotherm...
A time sequence of meridional baroclinic transport (0/1000 db) across the Subtropical gyre of the No...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Two data sets are used to reveal the quasi-stationary nature of the banded current structure in the ...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
Time series of baroclinic potential energy in the upper 500 meters of the North Pacific (20-50N, 145...
An array of 15 moorings with 33 current meters was deployed in the deep water across the Continental...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
Monthly mean values of temperature from both hydrographic and XBT casts are used to compute isotherm...