November 2014 Bering Sea cyclone

November 2014 Bering Sea cyclone
Post-Tropical Cyclone Nuri
The bomb cyclone at its peak intensity over the Bering Sea, on November 9, 2014
Meteorological history
FormedNovember 7, 2014
DissipatedNovember 13, 2014
Extratropical cyclone
Highest winds130 km/h (80 mph)
Lowest pressure920 hPa (mbar); 27.17 inHg[1]
(North Pacific extratropical record low)
Overall effects
FatalitiesNone reported
DamageUnknown
Areas affectedBering 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]

Meteorological history

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
circle Tropical cyclone
square Subtropical cyclone
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression