Construct · 1 fields · 1 citations
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Bombogenesis is the explosive intensification of an extratropical (midlatitude) cyclone, in which the storm's central pressure falls so fast that the system behaves like a winter equivalent of a hurricane in its rate of deepening. Sanders and Gyakum's 1980 Synoptic-dynamic climatology of the "bomb" gave the quantitative threshold still in use: a central-pressure drop of at least 24 hectopascals in 24 hours, geostrophically adjusted to a reference latitude of 60°, which they called a rate of one "bergeron". The referent is a rate of pressure fall in a developing cyclone, and the term is a meteorological coinage with no connection to explosives beyond the borrowed metaphor of something detonating.[1]
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