Here we show the existence of a distinctive seasonal cycle of subsurface cooling via mixing in the equatorial
Pacific cold tongue, using multi-year measurements of turbulence in the ocean.
Not exact matches
For the Ekman pumping (one good example of the Ekman pumping is the so - called «
cold tongue» near in the eastern part of the
Pacific near the Equator), the stability is not so important, but rather the depth of the upper warm surface layer.
In fact simultaneously with the strengthening warming of the subsurface western
Pacific is an intensification of the
cold subsurface
tongue at the east
Pacific (WUWT ENSO page).
Mixing of
cold, nutrient rich, sub-surface water with warm surface water creates the wind and current feedbacks drive the
cold tongue across the
Pacific.
Surface cloud forcing in the east
Pacific stratus deck /
cold tongue / ITCZ complex.