Large - scale
ocean circulation changes beyond the 21st century can not be reliably assessed because of uncertainties in the meltwater supply from the Greenland ice sheet and model response to the warming.
Not exact matches
Identify the impacts of a
changing climate on sea ice loss; sea ice loss on patterns of atmospheric
circulation and precipitation; oceanic
circulation both within and
beyond the Arctic, including the meridional overturning
circulation in the Atlantic
Ocean; and weather patterns in middle latitudes.
I have now realised that the global albedo
changes necessary and the
changes in solar energy input to the
oceans can be explained by the latitudinal shifts (
beyond normal seasonal variation) of all the air
circulation systems and in particular the net latitudinal positions of the three main cloud bands namely the two generated by the mid latitude jet streams plus the Inter Tropical Convergence Zone (ITCZ).