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November 2011 Bering Sea cyclone

Extratropical cyclone in East Asia and Alaska

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Through Atmospheric pressure

Meteorological synopsis

In early November 2011, an extratropical cyclone developed over the western Pacific Ocean. Gradually intensifying, the system moved rapidly northeastward at 60 mph (97 km/h) and reached the southern Aleutian Islands by November 8, with a barometric pressure estimated at 960 mbar (hPa; 28.35 inHg). Though still intensifying, winds associated with the storm were already estimated in excess of hurricane-force. By 9:00 p.m. AKST, the system had attained a pressure of around 943 mbar (hPa; 27.85 inHg) while it was near the Gulf of Anadyr. This made it one of the most powerful storms on record in the region, comparable to the November 1974 storm in Nome, Alaska, which was regarded as "the most severe in Nome in 113 years of record keeping." According to the National Weather Service (NWS), the system was forecast to have sustained winds of 80 mph (130 km/h) over an area the size of Colorado. After weakening somewhat, the storm crossed the Chukotsk Peninsula around 9:00 a.m. AKST on November 9 before moving over the Chukchi Sea later that day. Once back over water, the extratropical cyclone turned towards the northwest and was last noted as a 975 mbar (hPa; 28.80 inHg) low on November 10, about 150 mi (240 km) north of Wrangel Island, before dissipating on the next day.

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