This system involves the sinking of cold saline waters in the subpolar regions of the oceans, an action that helps to drive
warmer surface waters poleward from the subtropics.
Not exact matches
Warm and saline
water transported
poleward cools at the
surface when it reaches high latitudes and becomes denser and subsequently sinks into the deep ocean.
You wrote, «In addition to moving
warm Pacific
water poleward, the removal of the
warm Pacific tropical
surface waters exposes the atmosphere to huge amounts of cooler sub-
surface Pacific
water.
In addition to moving
warm Pacific
water poleward, the removal of the
warm Pacific tropical
surface waters exposes the atmosphere to huge amounts of cooler sub-
surface Pacific
water.
After the
warm surface waters have been stripped and pumped
poleward by the wind, the subsurface
waters are cooler than before.
The La Nina pump stroke moves
warm Pacific
surface water poleward to lose its heat through conduction, radiation, and evaporation.
Soon the eastern trade winds start pushing the
warm tropical
surface waters and their associated thunderstorms and clouds to the west across the Pacific and eventually
poleward again.