Geoscience Reference
In-Depth Information
Using the first three identities in the fourth term of Equation (18.8) and
rearranging gives:
2
2
2
2
∂′
()
w
∂′
()
w
∂′
()
w
∂′
()
w
(
w
′′
q
)
2(
∂′
w P
) 2
∂′
w
u
v
+
+
v
+
w
=
2
g
+
P
t
x
y
z
r
z
r
z
q
a
a
v
(18.11)
w
w
w
u
w
2
v
w
2
w
w
2
∂′
()
∂′
()
∂′
()
2(
wu
′ ′
)
+
2(
wv
′ ′
)
+
2(
ww
)
+
+
x
y
z
x
y
z
2
2
2
∂′
w
∂′
w
∂′
w
+
2
u
w
+′
w
+′
w
x
2
y
2
z
2
The product rule of calculus gives the results:
2
∂′
2
()
w
2
∂′
2
w
∂′
w
=′
w
+
x
w
2
x
x
2
∂′
2
()
2
∂′
2
w
∂′
w
(18.12)
=′
w
+
y
w
2
y
y
2
∂′
2
()
2
∂′
2
w
∂′
w
=′
w
+
z
2
z
z
but observations in the ABL show:
2
2
2
2
w
2
w
2
w
2
w
2
w
2
w
∂′
()
∂′
∂′
()
∂′
∂′
()
∂′
<<
;
<<
;
<<
(18.13)
2
x
2
y
2
z
x
y
z
Together Equations (18.12) and (18.13) imply that the last term in Equation
(18.11) can be re-written such that the equation becomes:
2
2
2
2
(
w
′′
)
∂′
()
w
∂′
()
w
∂′
()
w
∂′
()
w
q
2(
∂′
w P
) 2
∂′
w
+
u
+
v
+
w
=
2
g
v
+
P
r
r
t
x
y
z
z
z
q
a
a
v
(18.14)
w
w
w
∂ ′
u
()
w
2
∂ ′
v
()
w
2
w
(
w
2
(
wu
′ ′
)
+
(
wv
′ ′
)
+
(
ww
)
+
+
x
y
z
x
y
z
2
2
2
w
w
w
u
2
+
+
x
y
z
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