Thus as sea ice expands in a cooler climate, the high - latitude
oceanic heat loss to the atmosphere is inhibited, the thermohaline circulation weakens, and the sinking regions move equatorward, leading to a shallower and weaker deep circulation.
The oceanic heat loss depends of course on the sea surface temperature (SST).
Not exact matches
With a dominant internal component having the structure of the observed warming, and with radiative restoring strong enough to keep the forced component small, how can one keep the very strong radiative restoring from producing
heat loss from the oceans totally inconsistent with any measures of changes in
oceanic heat content?
''... how can one keep the very strong radiative restoring from producing
heat loss from the oceans totally inconsistent with any measures of changes in
oceanic heat content?»
Current events surrounding increased
oceanic heat around ice sheet margins in Antarctic are expected to play a dynamical role in marine terminating glacial ice
loss acceleration there as well.
Science Deliverable III From Deliverables I - II, predictions of (1) accelerating
oceanic heating, (2) accelerating ice - mass
loss, (3) accelerating incidence of extraordinary
heat and drought, (4) accelerating sea - level rise - rate.
I suspect that the number being used is a lower - bound for the amount of
heat released by the
oceanic crust because it represents the typical surface
heat loss of the great slabs of relatively cool basalt and gabbro.