TeachMeFinance.com - explain Pseudo-Cold Front
Pseudo-Cold Front The term 'Pseudo-Cold Front' as it applies to the area of the weather can be defined as ' A boundary between a supercell's inflow region and the rear-flank downdraft (or RFD). It extends outward from the mesocyclone center, usually toward the south or southwest (but occasionally bows outward to the east or southeast in the case of an occluded mesocyclone), and is characterized by advancing of the downdraft air toward the inflow region. It is a particular form of gust front'.
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