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
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.