Lecture 7, Dry Parcel Theory
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Transcript Lecture 7, Dry Parcel Theory
Convection: Parcel Theory
Chapt. 4 page 48.
• Vertical motion of parcels of air.
• Buoyant convection leads to the formation
of cumulus clouds (though other clouds
have convective features).
• Parcel theory is an elementary treatment,
but useful for qualitative understanding.
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
1
Parcel Theory Assumptions
• Parcel and environment are in dynamic
equilibrium: P = P’.
• Parcel maintains its identity; no mixing with
environment.
• Atmosphere in hydrostatic equilibrium.
• No compensating motion by atmosphere as
parcel moves.
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
2
Parcel theory equations:
d z
(T T ' )
z 2 g
dt
T'
2
or
z gB
with
T T
B
T
Primes: environmental properties.
You can correct for the effect
of moisture on density by using
virtual temperature wherever
T appears here.
Let B be buoyancy.
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
3
dz
U
dt
Designate updraft velocity
then
dU
z
dt
so
dz
dt
U
and
dU
z U
gB
dz
UdU gBdz
z
U 2 U o2 2 g B( z )dz
zo Dickerson
Copyright © 2009 R. R.
& Z.Q. Li
4
dP
g
dz
Alternate formulation using >>
= P’/R’T’ and dP’ = - gdz
(T T ) RT dP
2 g B ( z )dz 2 g
T
Pg
z
p
z
p
o
o
dP
2 R (T T )
P
p0
p
dP
2 R (T T )
P
p0
p
U
2
Uo
2
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
5
T’ (environment)
-RlnP
Parcel process curve
T
Hatched area is proportional to the kinetic energy of
the parcel. Change in area from level to level represents
the change in K.E.
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
6
Correcting for Condensed H2O
Let
mass of liquid
;
mass of air
assume μ= total adiabatic liquid water
dP
T
then z g (1 )
g (1 )
dz
T
Copyright © 2009 R. R. Dickerson
& Z.Q. Li
7
Parcel Theory is Useful for:
• Estimating cloud base and top heights
• Estimating stability
• Estimating vertical motion U
But we’ve neglected
• Drag
• Mixing
• Compensating motion by environment
• Effects of condensed water
Therefore: parcel Copyright
theory
U => expected upper limit.8
© 2009 R. R. Dickerson
& Z.Q. Li