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.

• National Weather Service Glossary

• Pseudo-warm front

This meteorology–related article is a stub. You can help Wikipedia by expanding it.

• v
• t
• e