Not exact matches
The
warm Atlantic water was saltier, and therefore heavier and
subducted at depth and reached to the bottom, actually heating up beneath a lid of ice and melt water, that prevented the release of heat to the atmosphere.
Some of the
warm water would be
subducted by Atlantic Meridional Overturning Circulation / Thermohaline Circulation, some would be carried by ocean currents into the Arctic Ocean where it would melt sea ice, and the remainder would be spun southward by the North Atlantic gyre toward the tropics so it could be
warmed more by the effects of the slower - than - normal trade winds.
As this heat moves counter-clockwise around the Arctic Ocean to the north of Siberia and Alaska, it
subducts, that is, it is covered by cold water that floats above the
warm Atlantic water.
However, it must be borne in mind that the MOC can also include shallower, wind - driven overturning cells such as occur in the upper ocean in the tropics and subtropics, in which
warm (light) waters moving poleward are transformed to slightly denser waters and
subducted equatorward at deeper levels.