Both hindcasts and projections are strongly influenced by climate sensitivity and also by
vertical ocean diffusivity.
Not exact matches
Hasumi, H., and N. Suginohara, 1999: Effects of locally enhanced
vertical diffusivity over rough bathymetry on the world
ocean circulation.
In particular, equilibrium climate sensitivity (S), effective
vertical deep
ocean diffusivity (Kv) and total aerosol forcing (Faer) have been estimated in this way.
This paper in Journal of Marine Research has nearly 500 citations and describes
vertical eddies in
ocean interior using
diffusivity as a metric.
Without winds or a high
vertical diffusivity, the
ocean does not support deep convection.