Add to ORKGUsing the equation of continuity, computations of the vertical velocity distribution in the upper ocean were made from moored horizontal current measurements recorded for 3 month intervals near 0 degree , 110 degree W. A depth-averaged upwelling velocity of 2.0 x 10 super(-5) m s super(-1) was characteristic of the Equatorial Undercurrent (EUC). Below the undercurrent, the mean vertical motion was directed downward. In the EUC the nonlinear advection was comparable to the westward force of the prevailing southeasterly winds
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The vertical structure of low frequency velocity and temperature variability in the eastern equatori...
Surface current measurements have been obtained from the Eastern tropical Pacific Ocean by means of ...
Using long-term current observations from 10 moorings in the central Pacific (1 degree 30'N)-1 degre...
Horizontal divergence and vertical velocity (w) are estimated at 0°, 140°W using an array of five su...
Vertical velocity on the equator in the western Pacific warm pool is investigated using data from th...
Current velocity data from an array of subsurface moorings deployed during the Tropical Instability ...
Upper-ocean horizontal velocity and divergence were estimated from shipboard observations taken from...
Simple scaling arguments conclude that the dominant motions in the ocean are horizontal. However, th...
The monitoring of upper ocean velocity, temperature, and surface winds at 0 degrees, 170 degrees W w...
Vertical velocity on the equator in the Central Pacific is estimated in four ways using mean CTD mea...
The monitoring of upper ocean velocity, temperature, and surface winds at 0°, 170°W was initiated in...
The annual cycle of the upper ocean\u27s vertical velocity component (w) on the equator at 28°W is e...
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The vertical structure of low frequency velocity and temperature variability in the eastern equatori...
Surface current measurements have been obtained from the Eastern tropical Pacific Ocean by means of ...
Using long-term current observations from 10 moorings in the central Pacific (1 degree 30'N)-1 degre...
Horizontal divergence and vertical velocity (w) are estimated at 0°, 140°W using an array of five su...
Vertical velocity on the equator in the western Pacific warm pool is investigated using data from th...
Current velocity data from an array of subsurface moorings deployed during the Tropical Instability ...
Upper-ocean horizontal velocity and divergence were estimated from shipboard observations taken from...
Simple scaling arguments conclude that the dominant motions in the ocean are horizontal. However, th...
The monitoring of upper ocean velocity, temperature, and surface winds at 0 degrees, 170 degrees W w...
Vertical velocity on the equator in the Central Pacific is estimated in four ways using mean CTD mea...
The monitoring of upper ocean velocity, temperature, and surface winds at 0°, 170°W was initiated in...
The annual cycle of the upper ocean\u27s vertical velocity component (w) on the equator at 28°W is e...
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The extratropical sources of equatorial undercurrent (EUC) water have been identified for an ocean c...
The vertical structure of low frequency velocity and temperature variability in the eastern equatori...