Not exact matches
Its measurements of
ocean saltiness will also help scientists understand
how changes in salinity affect the
deep currents that drive
ocean circulation.
«The weaker overturning
circulation brings less naturally CO2 - rich
deep waters to the surface, which limits
how much of that gas in the
deep ocean escapes to the atmosphere.
If somehow and I can't possibly imagine
how, there was a huge increase in
circulation between the surface and the
deeper layers of the
ocean, that would be disastrous for global temperatures but not upwards but downwards!
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.
Once the posts explaining the wind - driven
ocean circulation and
deep ocean warming are completed, it will be definitely worthwhile explaining
how all the pieces of the puzzle fit together.