Three-Dimensional Storm Structure and Low-Level Boundaries at Different Stages of Cyclic Mesocyclone Evolution in a High-Precipitation Tornadic Supercell

Figure 13

Same as Figure 4, except during the organizing stage of the third mesocyclone and the orientation has changed. The vertical velocity (panels (a), (c), and (e)) is from the perspective of looking at the storm from roughly the north. The vorticity (panels (b), (d), (f)) is from the perspective of looking at the storm from roughly the south.

(a)

(b)

(c)

(d)

(e)

(f)