There is so little understanding about how the ocean parses its response to forcings by 1) suppressing (local convective scale) deep water formation where
excessive warming patterns are changed, 2) enhancing (local convective scale) deep water formation where the changed
excessive warming patterns are co-located with
increased evaporation and
increased salinity, and 3) shifting favored deep water formation locations as a result of a) shifted patterns of enhanced warming, b) shifted patterns of enhanced salinity and c) shifted patterns of circulation which transport these enhanced ocean features to critically altered destinations.