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Kelvin wave

   Also found in: Wikipedia 0.01 sec.
Kelvin wave [′kelĀ·vən ‚wāv]
(oceanography)
An eastward-propagating internal gravity wave that crosses the Pacific Ocean along the equator and has no north-south velocity component.
A type of wave progression in relatively confined water bodies where, because of Coriolis force, the wave is higher to the right of direction of advance (in the Northern Hemisphere).


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h] V/[square root of (gh)] > 6 When this threshold is exceeded, the classical, linear Kelvin wave system is modified and specific, non-linear components of wakes frequently exist [31,32].
This oscillation is also partly linked to the Madden Julian Oscillation (MJO), which is a 30-60 day oscillation in tropical convection linked to an equatorially trapped Kelvin wave.
At the same time, the drop-off in the winds generates a fast-moving Kelvin wave that crosses the Pacific in 1 to 2 months.
 
 
 
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