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Contours of the vertical component of velocity due to buoyancy, ,
calculated using (7.25) and (7.35)
are shown in figure 7.2,
Figure 7.2:
Fully developed buoyancy-induced flow in various rectangular
sections. Curves can be interpreted as either vortex-lines or
contours of the vertical component of velocity with
levels at and of maximum.
and mark extrema of (points of
zero vorticity).
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in the unnormalized coordinates and . The curves can be
interpreted as either contours of or vortex-lines, since the gradient
of velocity in the -direction is zero (see Theorem 3,
p. ).
Geordie McBain
2001-01-27