a new parameterization of gravity waves for atmospheric ... · the scheme describes wave refraction...
TRANSCRIPT
A new parameterization of gravity waves foratmospheric circulation models based onthe radiative transfer equation
MATTHÄUS MAI, Erich BeckerLeibniz-Institute of Atmospheric Physics
LEIBNIZ-INSTITUTE OF ATMOSPHERIC PHYSICS | TRR 181 1
Solving the radiative transfer equation for Gravity Waves (GW) usingthe Gaussian variation principle
Radiative transfer equation [Olbers, Eden 2013 Journal of Physical Oceanography ]:
∂tE + ∂z (zE) + ∂m (mE) + ∂ωI(ωIE) =
ωI
ωI
E − m2DE + S (1)
Decomposition of spectral energy density: E(z, t, ωI ,m) = E0(z, t)A(m,m∗)B(ωI )
Assumptions/approximations:
Single columntextk = const
k = 0ω2
I = k2N2
m2ω2
I = k2N2
m2
Desaubies spectrumtextA(m,m∗) = NA
m/m∗1+(m/m∗)4
B(ωI ) = NBω−2
I
Mid-frequency, Boussinesq for GWtextω2
I = k2N2
m2
ω2
I = k2N2
m2
textDefinition of error squared:
χ2(z, t) :=
∫ ∫A(m,m∗)B(ω)
(radiative transfer equation
A(m,m∗)B(ω)
)2
dmdω
Variation ofχ2 with respect to ∂tE0(z, t) and ∂tm∗(z, t) yields the best approximate solution to the radiative transfer equation:
∂tE0 = +CE0∂zE0 + CE1∂zm∗E0 − CE2E0
∂zU
N+ CE3E0
∂zN
N− CE4DE0 + CE5S (2)
∂tm∗ = +Cm0
∂zE0E0
+ Cm1∂zm∗ − Cm2
∂zU
N+ Cm3
∂zN
N− Cm4D + Cm5
SE0
(3)
Ci = C∫∫
fi (m,m∗, ωI )dmdωI
LEIBNIZ-INSTITUTE OF ATMOSPHERIC PHYSICS | TRR 181 2
The Setting for the offline simulationWave field parameters: Background parameters: Dissipation by saturation:
Initial energy density:
0.0 0.1 0.2 0.30 in kg(ms2) 1
20
40
60
80
heig
ht in
km
Initial characteristic vertical wave number:
m∗(z, 0) = − 2π3000
m−1
Spectral parameters:
ωI ∈ [0.001826, 0.001916]s−1
m ∈[− 2π
10,− 2π
80000
]m−1
Source parameter:
S(z, t) = 0
Eastward mesospheric wind jet:
0 5 10 15 20U in ms 1
20
40
60
80
heig
ht in
km
Brunt-Väisälä frequency:
N(z, t) = 0.0187s−1
Density:
ρ(z) = 1.2 exp(−z/7000m)kgm−3
Static instability if:
1
ρN2
E0∫∫
m2A(m)B(ωI )dmdωI > α2
CDE0 > α2
When the lhs is bigger thanα2 the saturation isreached and dissipation sets in:
D = D0(CDE0 − α2)
case 1:
D0 = 0
case 2:
D0 = 100m2s−1
α2 = 0.5
LEIBNIZ-INSTITUTE OF ATMOSPHERIC PHYSICS | TRR 181 3
The scheme describes wave refraction and even critical layer (case1)
Horizontal wave propagation against the windjet, k < 0text text texttext text text
0 200 400 600 800time in min
20
40
60
80
heig
ht in
km
0 in 10 2kg(ms2) 1
0.01.22.43.64.86.07.28.49.6
0.020 0.015 0.010 0.005 0.000wave number in m 1
20
40
60
80
heig
ht in
km
m * at 500 min
Horizontal wave propagation in the direction of the windjet, k > 0
(critical layer)
0 200 400 600 800time in min
20
40
60
80
heig
ht in
km
0 in 10 2kg(ms2) 1
0.01.22.43.64.86.07.28.49.6
0.020 0.015 0.010 0.005 0.000wave number in m 1
20
40
60
80
heig
ht in
km
m * at 500 min
LEIBNIZ-INSTITUTE OF ATMOSPHERIC PHYSICS | TRR 181 4
The scheme describes wave refraction and even critical layer (case2)
Horizontal wave propagation against the windjet, k < 0text text texttext text text
0 200 400 600 800time in min
20
40
60
80
heig
ht in
km
0 in 10 2kg(ms2) 1
0.01.22.43.64.86.07.28.49.6
0.020 0.015 0.010 0.005 0.000wave number in m 1
20
40
60
80
heig
ht in
km
m * at 500 min
Horizontal wave propagation in the direction of the windjet, k > 0
(critical layer)
0 200 400 600 800time in min
20
40
60
80
heig
ht in
km
0 in 10 2kg(ms2) 1
0.01.22.43.64.86.07.28.49.6
0.020 0.015 0.010 0.005 0.000wave number in m 1
20
40
60
80
heig
ht in
km
m * at 500 min
LEIBNIZ-INSTITUTE OF ATMOSPHERIC PHYSICS | TRR 181 5