Geoscience Reference
In-Depth Information
dT
2
T
dx
2
T
dy
2
T
dz
2
T
dt
/ 2
+++
x
2
y
2
z
2
t
dt
dt
dt
dt
dt
(C.2)
2
T
2
T
2
T
2
T
u
v
w
=+++
,
2
x
2
y
2
z
2
t
or
2
T
dT
=− v
υ
$
d
T
.
(C.3)
2
t
dt
The last term in Eq. C.3 is called the advection term. It represents the influence
of the transport of heat to a location by the circulation. (See exercise 6.7.)
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