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.
Not exact matches
You've got the radiative physics, the measurements of ocean temperature and land temperature, the changes in ocean
heat content (Hint — upwards, whereas if if was just a matter of circulation moving
heat around you might expect something more simple) and of course observed predictions such as stratospheric cooling which you don't get when warming occurs from
oceanic circulation.
Over that period, solar forcing was net negative, volcanic forcing was net negative, and
oceanic fluctuations can not give the ocean
heat, merely shift it
around.
However, ENSO is an
oceanic cycle which merely moves
heat around between oceans and the surface, and thus can not cause a long - term warming trend.