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单词 bombogenesis
释义

bombogenesisn.

Brit. /bɒmbəˈdʒɛnᵻsɪs/, U.S. /ˌbɑmbəˈdʒɛnəsəs/, /ˌbɑmboʊˈdʒɛnəsəs/
Origin: Formed within English, by compounding. Etymons: bomb n., -o- connective, -genesis comb. form.
Etymology: < bomb n. + -o- connective + -genesis comb. form.
Meteorology.
A phenomenon or process characterized by a rapid and sustained fall of barometric pressure in the centre of an extratropical cyclonic weather system, indicative of the strengthening of the cyclone into a powerful storm; also called explosive cyclogenesis.
ΚΠ
1989 M. E. Adams Anat. ‘Bomb’ (M.Sc. thesis, N. Carolina State Univ.) 11 Climatology shows that a high frequency of ‘bombogenesis’ occurs over the ocean.
2019 Palm Beach (Florida) Post (Nexis) 16 Mar. a1 When a storm undergoes bombogenesis it means the counterclockwise spin of the low pressure system is creating a vacuum that drops atmospheric pressure by at least 24 millibars in 24 hours.
This is a new entry (OED Third Edition, December 2019; most recently modified version published online December 2021).
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n.1989
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