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- Q245472 subject Q7197713.
- Q245472 subject Q8275029.
- Q245472 abstract "Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low pressure area). Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale.Tropical cyclones form due to latent heat driven by significant thunderstorm activity, and are warm core.Extratropical cyclones form as waves along weather fronts before occluding later in their life cycle as cold core cyclones.Mesocyclones form as warm core cyclones over land, and can lead to tornado formation. Waterspouts can also form from mesocyclones, but more often develop from environments of high instability and low vertical wind shear.The process in which an extratropical cyclone undergoes a rapid drop in atmospheric pressure (24 millibars or more) in 24 hour period is referred to as explosive cyclogenesis, and is usually present during the formation of a nor'easter. The anticyclonic equivalent, the process of formation of high pressure areas, is anticyclogenesis. The opposite of cyclogenesis is cyclolysis.".
- Q245472 thumbnail Baroclinicleafphasecyclogenesiscropped.gif?width=300.
- Q245472 wikiPageWikiLink Q1022922.
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- Q245472 wikiPageWikiLink Q7197713.
- Q245472 wikiPageWikiLink Q7265294.
- Q245472 wikiPageWikiLink Q7347.
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- Q245472 wikiPageWikiLink Q812.
- Q245472 wikiPageWikiLink Q81242.
- Q245472 wikiPageWikiLink Q8275029.
- Q245472 comment "Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low pressure area).".
- Q245472 label "Cyclogenesis".
- Q245472 depiction Baroclinicleafphasecyclogenesiscropped.gif.
