The idea is that Arctic sea ice decline would expose the ocean to anomalous surface heat and freshwater fluxes, resulting in positive buoyancy anomalies that can propagate downstream to the North Atlantic, in due time
suppressing deep convection and weakening the AMOC.
Not exact matches
We suspect that water, the constituent of Saturn's
deepest cloud deck, can
suppress convection in the lighter hydrogen atmosphere for a period of decades, until finally buoyancy wins out and a large convective outburst ensues.
The links between model biases and the underlying assumptions of the shallow cumulus scheme are further diagnosed with the aid of large - eddy simulations and aircraft measurements, and by
suppressing the triggering of the
deep convection scheme.