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frontogenesis

[ fruhn-tuh-jen-uh-sis ]

noun

Meteorology.
  1. the formation or increase of a front or frontal zone.

frontogenesis

/ ˌfrʌntəʊdʒəˈnɛtɪk; ˌfrʌntəʊˈdʒɛnɪsɪs /

noun

  1. meteorol the formation or development of a front through the meeting of air or water masses from different origins
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

frontogenesis

/ ڰŭ′tō-ĕ′ĭ-ĭ /

  1. The formation or intensification of a meteorological front caused by an increase in the horizontal thermal gradient (the difference in temperature of adjacent air masses) over time.
  2. Compare frontolysis
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Derived Forms

  • ˌڰDzԳٴDzˈԱپ, adverb
  • frontogenetic, adjective
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yvlog History and Origins

Origin of frontogenesis1

First recorded in 1930–35; fronto- + -genesis

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