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The equatorial deep jets are often modeled as equatorially trapped long waves, either Kelvin or Rossby. Rossby waves perturb potential vorticity but Kelvin waves do not; therefore the potential vortic...
Equatorial deep jets are an unsolved mystery of the equatorial oceans. These alternating zonal currents appear steady over time spans of years, but no postulated energy source has proven plausible, an...
What drives the equatorial deep jets is a puzzle because of their isolation from surface forcing by the intervening main pycnocline and the Equatorial Undercurrent, and from lateral boundaries by dist...
The spatial and temporal structure of the equatorial deep jets (EDJs) in the Pacific Ocean is investigated using CTD station data taken on the equator from 1979 through 2001. The EDJs are revealed in ...
A simple linear theory of the circulation in a meridionally bounded equatorial ocean driven by density mixing localized near the eastern boundary is used to model the subthermocline circulation of the...
Vertical profiles of horizontal currents and hydrographic measurements from three cruises along 80.5°E from the coast of Sri Lanka to 6°S between December 1990 and September 1994 are used to investiga...
The so-called equatorial stacked jets are analyzed with ship-board observations and moored time series from the Atlantic Ocean. The features are identified and isolated by comparing vertical wavenumbe...

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