A pseudo-warm front is a boundary between the in-flow region and the forward-flank downdraft of a supercell. It can either be stationary or move in a northeasterly direction. [1] If it were …

Apr 17, 2023 · Pseudo-Warm Front A boundary between a supercell's inflow region and the forward-flank downdraft (or FFD). It extends outward from at or near the mesocyclone center, …

Pseudo-Warm Front A boundary between a supercell's inflow region and the forward-flank downdraft (or FFD). It extends outward from at or near the mesocyclone center, usually toward …

Pseudo-Warm Front A boundary between a supercell's inflow region and the forward-flank downdraft (or FFD). It extends outward from at or near the mesocyclone center, usually toward …

pseudo-warm front (forward -flank downdraft gust front). As with any inflow band, cloud elements move toward the updraft. Its size and shape change as the strength of the inflow changes.

Unlike the beaver tail, the tail cloud forms from air that is flowing from the storm's main precipitation cascade region (or outflow region). Thus, it can be oriented at a large angle to the …

Jan 19, 2024 · Warm fronts occur when a warm air mass advances and replaces a colder body of air, covering the colder air from the top and forcing the cold air out below. This type of front …

It is attached to a supercell's general updraft and is oriented roughly parallel to the pseudo-warm front, i.e., usually east to west or southeast to northwest. As with any inflow band, cloud …

Pseudo-Warm Front - A boundary between a 's region and the forward-flank (or FFD). It extends outward from at or near the , usually toward the east or southeast, and ly is either nearly …