Geoscience Reference
In-Depth Information
15.22 Why is the one-dimensional vorticity spectrum unusual? (Hint: sketch it.)
15.23 Interpret the argument of the function
f
in
Eq. (15.86)
as a squared ratio of
mean and turbulent strain rates.
15.24 Explain why the continuity constraint
u
i,i
=
0 prevents the isotropic form
of
φ
13
(
κ
)
,
Eq. (15.57)
, from vanishing.
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