Geoscience Reference
In-Depth Information
Answer 8
(a). Start from Equation (16. 46), the basic equation for conservation of water
vapor in the atmosphere, i.e.
S
q
q
q
q
2
q
2
q
2
q
E
q
+
u
+
v w
+
=
ν
+
+
+
+
q
t
x
y
z
x
2
y
2
z
2
rr
a
a
and expand the variables u, q and r a as mean and fluctuating part, thus:
(
qq
+′
)
(
qq
+′
)
(
qq
+′
)
(
qq
+′
)
++′
(
uu
)
++′
(
vv
)
+ +′
(
www
)
t
x
y
z
S
2
(
qq qq qq
+′
)
2
(
+′
)
2
(
+′
)
E
q
=
n
+
+
+
+
(
) (
)
q
2
2
2
x
y
z
rr
+′
rr
+′
a
a
a
a
Multiply out and separate the factors, thus:
q
q
q
q
q
q
q
q
q
q
+
+
u
+
u
+
u
'
+′
u
+
n
+
v
+′
v
+′
v
t
t
x
x
x
x
y
y
y
y
∂∂
S
q
q
q
q
2
2
2
2
2
2
q
q
q
q
q
q
E
q
wwww
z
+
+
+′
+′
=
n
+
+
+
+
+
+
+
(
) (
)
q
z
z
z
x
2
x
2
y
2
y
2
z
2
z
2
rr
+′
rr
+′
a
a
a
a
Average this equation and apply the Boussinesq approximation (in this case this just
means using average values for density because there is no buoyancy term), thus:
∂∂
qq q q q q qq q q
u
∂ ∂
+
+
+
u
+
u
+
u
+
n
+
v
+
v
+
v
∂∂
t
t
x
x
x
x
∂ ∂
y
y
y
y
S
q
q
q
q
2
q
2
q
2
q
2
q
2
q
2
q
E
q
+
wwww
z
+
+
+
=
n
+
+
+
+
+
+
+
q
2
2
2
2
2
2
z
z
z
x
x
y
y
z
z
rr
a
a
Apply Reynolds averaging to eliminate terms 2, 4, 5, 8, 9, 12, 13, 16, 18, and 20 and
to eliminate overbars on already averaged terms, thus:
S
2
2
2
q
q
q
q
q
q
q
q
q
q
E
⎡⎤ +
q
u
+
u
+
n
+
v ww
+
+
=
n
+
+
+
+
⎢⎥
⎣⎦⎢
q
t
x
x
y
y
z
z
2
2
2
x
y
z
rr
a
a
Re-order the terms and rewrite the viscosity term in vector format, thus:
S
q
q
q
q
E
q
q
q
q
2
+ + +
u
v w q
=∇++−′
n
.
u
+′
v w
+′
q
t
x
y
z
x
y
z
rr
a
a
 
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