November 2014 Bering Sea cyclone
The bomb cyclone at its peak intensity over the Bering Sea, on November 9, 2014 | |
| 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 (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 |
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. 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.