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Two-Dimensional Dynamics of Ice Crystal Parcels in a Cirrus Uncinus Cover

Two-Dimensional Dynamics of Ice Crystal Parcels in a Cirrus Uncinus

Open Access
|Jul 2023

Figures & Tables

Table 1

Nomenclature.

SYMBOLMEANING
ACrystal area (m2)
aHexagonal column crystal radius (m)
BiTotal radiance of black body (W m–2)
cHexagonal column crystal half-length (m)
cBHexagonal column crystal core half-length (m)
cpaSpecific heat of dry air (J K–1 kg–1)
CCapacitance of the ice crystal (m)
CDDrag coefficient
CpPhase speed of oscillations (m s–1)
DiEquivalent diameter of ice particle (m)
DvDiffusivity of water vapour in air (m2 s–1)
fvVentilation coefficient
Fu, FdUpward, downward radiative flux densitities (W m–2)
gGravity field constant (g = 9.81 m s–2)
HlRelative humidity of water vapour over liquid water
HiRelative humidity of water vapour over ice
tellusa-75-1-3227-g42.pngHeating rate (K d–1)
IWPIce Water Path (g m–3)
kDamping coefficient (s–1)
KaHeat conductivity of ambient dry air (W K–1 m–1)
LsLatent heat of sublimation of ice (Ls = 2.837 × 106 J kg–1)
LvLatent heat of vaporization of water (Lv = 2.525 × 106 J kg–1)
mCrystal mass (kg)
PPeriod of oscillatory motion (s)
pTotal pressure (Pa)
prReference pressure (pr = 105 Pa)
paPartial pressure of dry air (Pa)
pvPartial pressure of water vapour (Pa)
pvslSaturation pressure of water vapour over liquid water (Pa)
pvsiSaturation pressure of water vapour over ice (Pa)
qsSaturation mixing ratio (kg kg–1)
QabsEfficiency factor for absorption of radiation (Qabs ≈ 1)
riEquivalent radius of ice crystal (m)
Source term in radiative contribution (W)
RRadiative term in the mass equation (%)
RaGas constant of dry air (Ra = 287.05 J K–1 kg–1)
RvGas constant of water vapour (Rv = 461.00 J K1 kg–1)
ReReynolds number
RiRichardson number
SlSaturation ratio of water vapour over liquid water
SiSaturation ratio of water vapour over ice
TAbsolute temperature (K)
TrReference temperature (Tr = 273.15 K)
TaTemperature of ambient air (K)
TsTemperature of crystal surface (K)
u, wComponents of crystal velocity (m s–1)
Ua, WaComponents of ambient air velocity (m s–1)
VCrystal volume (m3)
WfFree-fall speed (m s–1)
Wf∞Terminal free-fall speed (m s–1)
x, zCartesian coordinates of ice crystal (m)
za0Critical altitude of horizontal wind (m)
zw0Critical altitude of updraft (m)
αCoefficient in Eq. (27)
εRatio of gas constants Ra/Rv (ε = 0.622)
ζDamping ratio
ηRadiative transfer ratio
θLatitude
θd, θePotential temperature (dry, equivalent)
ΛWavelength of oscillatory motion (m)
 
μaDynamic viscosity of air (Pa s)
ρaMass density of dry air (kg m–3)
ρMass density of wet air (kg m–3)
ρiMass density of ice (ρi = 920 kg m–3)
σStefan-Boltzmann constant (σ = 5.67 × 10–8 W m–2 K–4)
σSVertical gradient of ice supersaturation (m–1)
τNon-dimensional time of analytic model
τDDrag relaxation time (s)
ϕAspect ratio (ϕ = c/a)
ψHollowness factor (ψ = 1–cB/c)
ωWind shear (m s–1 km–1 or s–1)
ΩAngular frequency of oscillations (= 2π/P) (rad s–1)
Ω0Rotation rate of the Earth (Ω0= 7.27 × 10–5 rad s–1)
ΩBVBrunt-Väisälä angular frequency (rad s–1)
Figure 1

Atmospheric profile of horizontal wind.

Figure 2

Atmospheric profiles of vertical wind.

Figure 3

Atmospheric profiles of temperature and pressure of dry air.

Figure 4

Atmospheric profiles of relative humidity and saturation ratios.

Figure 5

Atmospheric profile of atmospheric infrared ratio ηa.

Figure 6

The shape of the mean crystal (meridian and axial cross sections) (after Chen and Wang, 2009).

Table 2

Parameters of test-cases/numerical experiments.

CASE NB0123
NET RAD. TRANSF.R ≠ 0R = 0R ≠ 0R ≠ 0
Parameterη(z)
ϕ = ϕ0
cB = cB0
η = η0 = 1
ϕ = ϕ0
cB = cB0
η = η0 ≠ 1
ϕ = ϕ0
cB = cB0
η = η0 ≠ 1
ϕ = ϕ0
cB = cB0
ModesSteady – OscSteady – Osc(Steady) – Osc(Steady) – Osc
Life time5 h/40 h5 h/40 h4 h/40 h4 h/40 h
∆t (s)0.02/0.040.02/0.040.02/0.040.02/0.04
x0 (km)2222
z0 (km)10101010
u0 (m s–1)0000
w0 (m s–1)0.60.60.80.8
a0 (μm)51.150.1752.050.2
c0 (μm)102.2100.34104.0100.4
ϕ02.02.02.02.0
ψ00.800.800.800.80
cB0 (μm)20.4420.06820.8020.08
m0 (μg)0.9350.8850.9860.887
C0 (μm)88.686.990.187.0
D0 (μm)125122127123
ρie0 (kg m–3)675675675 
η0.9 ≤ η ≤ 1.111.10.9
0 (km)9 ≤ z ≤ 100 – 110 – 110 – 11
Wa0 (m/s)0.60.60.80.8
zW0 (km)10/910/910/710/7
Ha30.610.610.680.68
zH3 (km)10101010
zmax0z0 (m)102144468542
z(km)9.639.588.588.3
P (hour)10.28.877.86.8
Λ (km)69.864.8200200
Cp (m s–1)1.852.037.18.2
ζ0.0190.0150.0210.011
Figure 7

Profiles of the parcel trajectory and hodograph (z0 = 10 km; zw0 = 10 km).

Figure 8

Time profiles of abscissa and altitude (zw0 = 10 km).

Figure 9

Time profiles of free-fall speed Wf and driving factor Si–1–R (zw0 = 10 km).

Figure 10

Profiles of ice supersaturation Si–1 and radiative correction R (zw0 = 10 km).

Figure 11

Profiles of crystal’s mass and dimensions (zw0 = 10 km).

Figure 12

Profiles of mass equivalent diameter and dynamic viscosity (zw0 = 10 km).

Figure 13

Profiles of hollowness factor and effective mass density of crystal (zw0 = 10 km).

Figure 14

Profiles of drag coefficient and Reynolds number (zw0 = 10 km).

Figure 15

Time profiles of damping coefficient and temperature difference ice-air (zw0 = 10 km).

Figure 16

Profiles of the parcel trajectory and hodograph (z0 = 10 km; zw0 = 9 km).

Figure 17

Time profiles of abscissa and altitude (zw0 = 9 km).

Figure 18

Time profiles of free-fall speed Wf and driving factor Si–1–R (zw0 = 9 km).

Figure 19

Time profiles of ice supersaturation Si-1 and radiative correction R (zw0 = 9 km).

Figure 20

Time profiles of mass m and dimensions a, c, cB (zw0 = 9 km).

Figure 21

Time profiles of mass equivalent diameter and dynamic viscosity (zw0 = 9 km).

Figure 22

Time profiles of hollowness factor and effective mass density of crystal (zw0 = 9 km).

Figure 23

Time profiles of drag coefficient CD and Reynolds number Re (zw0 = 9 km).

Figure 24

Time profiles of damping coefficient k and temperature difference ice-ambient air (zw0 = 9 km).

Figure 25

Profiles of falling height z20z0 and maximum height in the head zMz0 as functions of crystal half-width a0 (zw0 = 10 km).

Figure 26

Profiles of transit times t10, t20 and half-lengths c10/c0 and c20/c0 as functions of crystal half-width a0 (zw0 = 10 km).

Figure 27

Profiles of pseudo-periods between minima (Pmin) and maxima (Pmax) estimated with Eq. (53), as functions of crystal half-width a0 (zw0 = 9 km).

Figure 28

Profiles of wavelengths Λmin and Λmax derived from distances of minima and maxima by Eq. (54) as functions of crystal half-width a0 (zw0 = 9 km).

Figure 29

Profiles of phase speeds Cpmin and Cpmax derived by Eq. (55) as functions of crystal half-width a0 (zw0 = 9 km).

Figure 30

Profiles of relative altitudes at minima and maxima in the trail as functions of crystal half-width a0 (zw0 = 9 km).

Figure 31

Profiles of relative limit height zz0 and velocity Ua(z) in the trail as functions of crystal size a0 (zw0 = 9 km).

Figure 32

Profiles of the parcel trajectory, hodograph, altitude, supersaturation (η = 1; Wa = 0.6 m/s; Ha3 = 61%; zw0 = 9 km).

Figure 33

Profiles of the parcel trajectory, hodograph, altitude, supersaturation Si –1, driving factor Si –1–R and radiative correction R (η = 1.1; Wa = 0.8 m/s; Ha3 = 68%; zw0 = 7 km).

Figure 34

Time profile of the horizontal velocity u (η = 1.1; Wa = 0.8 m/s; Ha3 = 68%; zw0 = 7 km).

Figure 35

Profiles of the parcel trajectory, hodograph, altitude, supersaturation Si –1, driving factor Si –1–R and radiative correction R (η = 0.9; Wa = 0.8 m/s; Ha3 = 68%; zw0 = 7 km).

Figure 36

Time profile of the horizontal velocity u (η = 0.9; Wa = 0.8 m/s; Ha3 = 68%; zw0 = 7 km).

Figure 37

Atmospheric profiles of Richardson numbers.

Figure 38

Qualitative time profile of analytical free fall speed.

Figure 39

Trajectory and hodograph for analytic solution, Eq.(99).

Figure 40

Time profile of free fall speed for analytic solution, Eq.(99).

Figure 41

Altitude time profile of theoretical underdamped harmonic oscillator, Eq.(118) for moderate (a) and strong (b) damping.

Table 3

Parameters of theoretical periodic profiles.

DAMPINGMODERATESTRONG
z0 (km)10.010.0
z (km)9.638.58
P (hour)10.27.8
0 (rad s–1)1.71 × 10–42.24 × 10–4
ζ0.050.07
Φ (rad)π/4π/4
Language: English
Page range: 231 - 270
Submitted on: Dec 22, 2022
Accepted on: Jun 17, 2023
Published on: Jul 18, 2023
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2023 Roland P. H. Berton, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.