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mesoscale convective vortex
A mesoscale convective vortex (MCV) is a low-pressure center within an mesoscale convective system (MCS) that pulls winds into a circling pattern, or vortex. With a core only 30 to wide and 1 to deep, an MCV is often overlooked in standard weather analysis . But an MCV can take on a life of its own, persisting for up to 12 hours after its parent MCS has dissipated. This orphaned MCV will sometimes then become the seed of the next thunderstorm outbreak. An MCV that moves into tropical waters, such as the Gulf of Mexico, can serve as the nucleus for a tropical storm or hurricane.
== May 2009 Mid-Mississippi Valley MCV ==
(詳細はCarbondale, Illinois.〔http://www.crh.noaa.gov/news/display_cmsstory.php?wfo=pah&storyid=27320&source=0〕〔http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/05/090508_g12_ir_anim.gif〕〔http://www.register-news.com/local/local_story_128234308.html〕〔http://blogs.chron.com/sciguy/archives/2009/05/midwest_experie.html〕
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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