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second-order closure models are developed and then applied to the problem. Recently, several
papers have been published focusing on the closure problem, particularly within forest
canopies [26-28]. However, because the traditional K-theory approach can be applied
successfully within tall grass canopies [21], we shall stay with it.
A number of assumptions are offered about the variation of K s within tall grass canopies
[29,30]. Among those, we chose the approach where K s is proportional to wind speed, u , i.e.,
K s
=
σ
u
,
(17)
where the scaling length, σ , is an arbitrary, unknown constant. Combining Eqs. (11) and (17)
produces an equation for the wind speed inside the canopy
(
) 2
2
2
d
u
2
C
L
H
h
d
d
=
u
.
(18)
2
σ
H
dz
A particular solution of this equation can be found in a form that approximates the wind
profile within the tall grass canopy fairly well [31]:
1
z
u
(
z
)
=
u
(
H
)
exp
β
1
(19)
2
H
where u ( H ) is the wind speed at the canopy height and β is the extinction parameter, defined
as
(
)
2
L
H
h
H
2
d
d
β
=
,
(20)
σ
where σ still remains an unknown constant. Its value can be determined as a function of the
morphological and aerodynamic characteristics of the underlying tall grass canopy in the
following manner. We shall use the lower boundary condition at the canopy bottom z = h in
terms of the shear stress, τ , just above and below the indicated level. Therefore,
2
τ =
ρ
u
,
(21)
dg
h
h
where C dg is the leaf drag coefficient estimated from the size of the roughness elements of the
ground [21], i.e.,
2
k
C
=
,
(22)
dg
2
h
ln
z
g
where k is the von Karman constant, taken to be 0.41, and
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