Assessment of decadal variability in sea ice in the community earth system model against a long-term regional observational record: Implications for the predictability of an ice-free arctic

Abstract

Uncertainties in the timing of a seasonal ice cover in the Arctic Ocean depend on model physics and parameterizations, natural variability at decadal time scales, and uncertainties in climate scenarios and forcings. We use the Gridded Monthly Sea Ice Extent and Concentration, 1850 Onward data product to assess the simulated decadal variability from the Community Earth System Model-Large Ensemble (CESM-LE) in the Pacific, Eurasian, and Atlantic sectors of the Arctic where a longer observational record exists. Results show that sea ice decadal (8-16 years) variability in CESM-LE is in agreement with the observational record in the Pacific sector of the Arctic, underestimated in the Eurasian sector of the Arctic, specifically in the East Siberian Sea, and slightly overestimated in the Atlantic sector of the Arctic, specifically in the Greenland Sea. Results also show an increase in variability at decadal time scales in the Eurasian and Pacific sectors during the transition to a seasonally ice-free Arctic, in agreement with the observational record although this increase is delayed by 10-20 years. If the current sea ice retreat in the Arctic continues to be Pacific-centric, results from the CESM-LE suggest that uncertainty in the timing of an ice-free Arctic associated with natural variability is realistic, but that a seasonal ice cover may occur earlier than projected.