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Pseudo-cold front
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Pseudo-cold front : ウィキペディア英語版
Pseudo-cold front
In meteorology, a pseudo-cold front is a boundary between a supercell's inflow region and the rear flank downdraft. It usually extends outward from a mesocyclone center, usually toward the south or southwest, and is characterized by advancing of the downdraft air toward the inflow region. It is a particular form of gust front.
==References==

*(National Weather Service Glossary )

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Pseudo-cold front」の詳細全文を読む



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