Ensemble decadal prediction simulations using the Community Earth System Model (CESM) can skillfully predict
past decadal rates of Atlantic winter sea ice change because they do well at predicting THC - driven ocean heat content change in the vicinity of the winter sea ice edge in the Labrador, Greenland, Irminger, and Barents Seas.
Not exact matches
Despite large year - to - year variability of temperature,
decadal averages reveal isotherms (lines of a given average temperature) moving poleward at a typical
rate of the order of 100 km / decade in the
past three decades [101], although the range shifts for specific species follow more complex patterns [102].
Despite large year - to - year variability of temperature,
decadal averages reveal isotherms (lines of a given average temperature) moving poleward at a typical
rate of the order of 100 km / decade in the
past three decades [101], although the range shifts for specific species follow more complex patterns [102].