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Abstract Over the past 40 years, the Arctic sea ice minimum in September has declined. The period between 2007 and 2012 showed accelerated melt contributed to the record minima of 2007 and 2012. Here, observational and model evidence shows that the changes in summer sea ice since the 2000s reflect a continuous anthropogenically forced melting masked by interdecadal variability of Arctic atmospheric circulation. This variation is partially driven by teleconnections originating from sea surface temperature (SST) changes in the east-central tropical Pacific via a Rossby wave train propagating into the Arctic [herein referred to as the Pacific–Arctic teleconnection (PARC)], which represents the leading internal mode connecting the pole to lower latitudes. This mode has contributed to accelerated warming and Arctic sea ice loss from 2007 to 2012, followed by slower declines in recent years, resulting in the appearance of a slowdown over the past 11 years. A pacemaker model simulation, in which we specify observe📍 Venue: High Noon Saloon
🏠 Address: 701 E. Washington Ave
🗺️ Extended Address: Madison, WI 53703
🌆 City: Madison
📍 Location: 43.0796, -89.3765Error occurred: DateTime::__construct(): Failed to parse time string (High Noon Saloon) at position 0 (H): The timezone could not be found in the database
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Event Venue & Nearby Stays
High Noon Saloon, 701 E. Washington Ave, Madison, WI 53703, US, United States
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