Chapter 5.3.2 Right-moving multicell storms

Note the vertical shear of the horizontal winds, a clockwise turning (veering) with height (Figure 5.24)

Because of the veering of wind with height the low-level moisture feed occurs along the southern flank of the storm

Cells on the north side begin to decay as their moisture source is intercepted (Figure 5.24)

Note the vertical shear of the horizontal winds, a clockwise turning (veering) with height (Figure 5.24)