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. See also pseudo-warm front.
PSEUDO-COLD FRONT
Meaning of PSEUDO-COLD FRONT in English
Weather and meteorology English vocabulary. Английский словарь погоды и метеорологии . 2012