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This study investigates a significant sea-ice volume anomaly in the Northern Hemisphere, lasting about 20 years and reaching 8.6 x 10^3 km3, triggered by specific atmospheric circulation patterns. The anomaly is linked to surface cooling and changes in oceanic convection, which amplify the cooling effect and influence the ice volume. The frequency of such events is sensitive to the mean climate conditions simulated by the model, with a higher occurrence in colder climates.

Author

abdelmoneim.w.elhawary

Language

EN