Rapidly deepening extratropical cyclonic low-pressure area
This article is about extratropical cyclones. For tropical cyclones, see Rapid intensification.
Explosive cyclogenesis (also referred to as a weather bomb,[1][2][3]meteorological bomb,[4]explosive development,[1]bomb cyclone,[5][6] or bombogenesis[7][8][9]) is the rapid deepening of an extratropical cyclonic low-pressure area. The change in pressure needed to classify something as explosive cyclogenesis is latitude dependent. For example, at 60° latitude, explosive cyclogenesis occurs if the central pressure decreases by 24 millibars (0.71 inHg) or more in 24 hours.[10][11] This is a predominantly maritime, winter event,[10][12] but also occurs in continental settings.[13][14] This process is the extratropical equivalent of the tropical rapid deepening. Although their cyclogenesis is entirely different from that of tropical cyclones, bomb cyclones can produce winds of 74 to 95 mph (120 to 155 km/h), the same order as the first categories of the Saffir–Simpson scale, and yield heavy precipitation. Even though only a minority of bomb cyclones become this strong, some weaker ones can also cause significant damage.
^ ab"Fierce 'weather bomb' batters Britain". The Telegraph. 9 December 2011. Archived from the original on 9 December 2011. Retrieved 21 March 2013.
^"The worst storm in years?". Met Office Blog. 28 January 2013. Retrieved 21 March 2013.
^Edwards, Tim (9 December 2011). "Scotland storm: what is a weather bomb?". The Week. London, United Kingdom: Dennis Publishing. Retrieved 4 April 2013.
^O'Hanlon, Larry (25 February 2013). "Look out -- 'meteorological bomb' is on the way!". NBC News. Retrieved 21 March 2013.
^Williams, Jack (20 May 2005). "Bomb cyclones ravage northwestern Atlantic". USA Today. Retrieved 22 March 2013.
^Feltman, Rachel (3 January 2018). "What the heck is a bomb cyclone?". Popular Science. Retrieved 6 January 2018.
^"Ryan explains Bomb Cyclogenesis". WBRZ News 2 Louisiana. Archived from the original on 12 April 2013. Retrieved 21 March 2013.
^Freedman, Andrew (1 March 2013). "Meteorological bomb explodes over New England". Washington Post. Retrieved 21 March 2013.
^Rodman, Kristen (23 January 2014). "What is Bombogenesis?". Accuweather. Retrieved 31 January 2014.
^ abSanders, Frederick; Gyakum, John R (1980). "Synoptic-Dynamic Climatology of the 'Bomb'". Monthly Weather Review. 108 (10): 1589–606. Bibcode:1980MWRv..108.1589S. doi:10.1175/1520-0493(1980)108<1589:SDCOT>2.0.CO;2.
^Chelsea Harvey (November 10, 2014). "Here's What Caused The 'Bomb Cyclone' That's About To Freeze The Northern US". Business Insider. Retrieved October 8, 2017.
^Cite error: The named reference AMS_Glossary_20120220 was invoked but never defined (see the help page).
^"The Bomb". blog.ametsoc.org. 27 October 2010. Retrieved 21 March 2013.
^MacDonald, Bruce C; Reiter, Elmar R (1988). "Explosive Cyclogenesis over the Eastern United States". Monthly Weather Review. 116 (8): 1568–86. Bibcode:1988MWRv..116.1568M. doi:10.1175/1520-0493(1988)116<1568:ECOTEU>2.0.CO;2.
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