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where z r is a reference height and a is the power law exponent (sometimes called
“Hellmann exponent”). a depends on surface roughness and the thermal stability
of the Prandtl layer. (A comparison of eqs. ( 2.5 ) and ( 2.5a )isdiscussedinEmeis
( 2005 ).) The wind speed increases with height without a turning of the wind direc-
tion. A scale analysis gives for the height of the Prandtl layer z p (Kraus 2008 ):
0.00064 v g
f
0.01 u
f
z p
.
(2.6)
Putting in numbers ( u =
=
/
=
0.5 m/s, f
0.0001 1
s , v g
8 m/s) gives a typical
height of the Prandtl layer of 50 m.
In a well-mixed Prandtl layer, the temperature T is decreasing with height accord-
ing to the adiabatic lapse rate, g/c p ( g is gravity acceleration, c p is specific heat at
constant pressure). The potential temperature,
p ) R / c p is constant with
=
T ( p 0 /
height ( R is the gas constant for dry air).
The standard deviations of the three velocity components ( u denotes the stream-
wise component, v crosswise, w vertical) are independent of height and scale with
the friction velocity (Stull 1988 ,Arya 1995 ):
σ u
u
σ v
u
σ w
u
2.5;
1.9;
1.3.
(2.7)
The turbulence intensity in the streamwise direction decreases with height due to
the increase of the mean wind speed with height. By inserting the left-hand relation
from eq. ( 2.7 ) into eq. ( 2.5 ), we get (Wieringa 1973 )
σ u
u ( z ) =
1
ln( z
z 0 ) .
(2.8)
/
2.2.1.2 Ekman Layer
The Ekman layer covers the major part of the ABL above the Prandtl layer. If the
simplifying assumption is made that the height-dependent growth of the exchange
coefficient K M stops at the top of the Prandtl layer and that it is vertically constant
within the Ekman layer, we can solve eqs. ( 2.1 ) and ( 2.2 ) analytically for the wind
profile in the Ekman layer:
u ( z )
=
u g (1
exp(
γ
z ) cos
γ
z ),
(2.9)
v ( z )
=
u g exp(
γ
z )sin
γ
z ,
(2.10)
f
γ =
/
where
(2 K M ). Equation ( 2.9 ) describes the well-known “Ekman spiral.”
The height of the Ekman layer is estimated by
z E = π
γ
(2.11)
 
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