Geoscience Reference
In-Depth Information
R
t
¼
R
u
ð
c
teff
Þ
R
u
ð
c
s
;
h
Þ
ð
6
:
17
Þ
using R
u
(c
s,h
) = u
h0
/u
0
. Inserting for the exchange coefficient K
m
(
6.9
) and the
effective drag coefficient (
6.15
)in(
6.7
) yields:
c
teff
u
h
¼
ju
zu
0
u
h
ð
Þ
ð
6
:
18
Þ
Dz/
m
The height z in (
6.18
) is essentially h ? Dz, so that the ratio z/Dz can be
approximated by a constant value:
z
Dz
¼
f
h
;
Dz
ð
6
:
19
Þ
The horizontal turbulence intensity I
u
at hub height h is defined by:
I
u
¼
r
u
u
h
ð
6
:
20
Þ
The standard deviation of the horizontal wind speed can be parameterized using
the friction velocity u
*
:
r
u
¼
1
j
u
ð
6
:
21
Þ
which yields the following relation between friction velocity, u
*
and turbulence
intensity, I
u
:
u
¼
jr
u
¼
ju
h
I
u
ð
6
:
22
Þ
Inserting of (
6.19
) and (
6.22
)in(
6.18
) yields finally:
c
teff
u
h
¼
j
2
u
h
u
0
u
h
f
h
;
Dz
I
u
¼
j
2
u
h
u
0
u
0
/
m
f
h
;
Dz
I
u
j
2
u
h
/
m
ð
Þ
f
h
;
Dz
I
u
ð
6
:
23
Þ
/
m
Rearrangement leads to:
¼
u
0
c
teff
u
h
þ
j
2
u
h
/
m
c
teff
þ
j
2
/
m
R
u
j
2
/
m
f
h
;
Dz
I
u
¼
u
h
f
h
;
Dz
I
u
f
h
;
Dz
I
u
ð
6
:
24
Þ
and finally to an expression for the ratio (
6.16
):
j
2
/
m
f
h
;
Dz
I
u
c
teff
þ
j
2
R
u
¼
u
h
u
0
u
h
R
u
u
0
f
h
;
Dz
I
u
f
h
;
Dz
I
u
þ
/
j
2
c
teff
¼
¼
¼
ð
6
:
25
Þ
/
m
f
h
;
Dz
I
u
Thus, the ratio (
6.17
) between the wind speed at hub height inside the wind park
to the undisturbed wind speed upstream is:
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