Meteorological history | |
---|---|
Formed | November 7, 2014 |
Dissipated | November 13, 2014 |
Extratropical cyclone | |
Highest winds | 130 km/h (80 mph) |
Lowest pressure | 920 hPa (mbar); 27.17 inHg[1] (North Pacific extratropical record low) |
Overall effects | |
Fatalities | None reported |
Damage | Unknown |
Areas affected | Bering Sea, Aleutian Islands, Russian Far East, Alaska, Contiguous United States[2] |
Part of the 2014–15 North American winter |
The November 2014 Bering Sea cyclone (also referred to as Post-Tropical Cyclone Nuri by the U.S. government) was the most intense extratropical cyclone (also a bomb cyclone) ever recorded in the Bering Sea, which formed from a new storm developing out of the low-level circulation that separated from Typhoon Nuri, which soon absorbed the latter.[3][4][5][6] The cyclone brought gale-force winds to the western Aleutian Islands and produced even higher gusts in other locations, including a 97 miles per hour (156 km/h) gust in Shemya, Alaska. The storm coincidentally occurred three years after another historic extratropical cyclone impacted an area slightly further to the east.[4]