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High-resolution Observations and Model Simulations of the Life Cycle
of an Intense Mesoscale Snowband over the Northeastern United States
Reporter: Prudence Yi-Yun Chien
Reference:
Novak, D. R., B. A. Colle, and S. E. Yuter, 2008: High-resolution Observations and Model Simulations of the Life Cycle of an Intense Mesoscale Snowband over the Northeastern United States. Mon. Wea. Rev., 136, 1433–1456.
2
Outline
• Key words
• Introduction
• Datasets and methodology
• Case overview
• Band life cycle
• Moisture availability
• Summary and discussion
2
3
Key words
yy
v
xy
u
yyx
v
xx
u
x
dt
dF D
1
2
2D form of frontogenesis equation (Miller, 1948)
Assess frontal forcing for ascent F2D > 0
3
4
Key words
esgEPV Saturation equivalent potential vorticity (EPV)
θes surface slope > M surface slope
EPV<0Saturation environment
0
0
EPVfzgyMf
yMf
eses
es
1→2
Conditional Symmetric instability
CSI condition:
4
0
0
y
Mzes Conditional stable
Inertial stable, M = fy-ug
5
Introduction
• Motivation:Advance cool-season QPF=> Structural and dynamical evolution of a cool-season mesoscale snowband
• Using high-resolution obs. & model
• Case period: 2002/12/25~ 2002/12/26
5
6
Datasets and methodology
Dual-Doppler synthesis
1. Upper-air obs2. Doppler radar3. Wind profiler4. ground-based integrated
precipitable water vapor (IPW)5. Conventional surface obs6. Commercial aircraft
Observation
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MM5 V3.4
Cumulus Grell (1993)
Microphysics Dudhia (1989)
PBL MRF
IC NCEP - EDAS analysis (0000UTC 25 Dec)
BC NCEP – Eta forcast (0000UTC 25 Dec)
SST US Navy OTIS
Model configurations
31 sigma levels
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Case overview
• Synoptic-scale evolution
• Mesoscale evolution
• QPF
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9
Synoptic-scale evolution
500-hPa Φ(solid)
300-hPa wind (barb)
IR brightness temperature (shaded)
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Synoptic-scale evolution
isobars (solid)
isotherms (gray)
wind (barb) 10
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Mesoscale evolution
700-hPa Φ (thick solid)
F2D (thin solid)
reflectivity (shaded)
MM51800UTC 12/25
2760m2790m
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Mesoscale evolution
700-hPa θ (thick solid)
F2D (shaded)
wind (barb)
MM5 700-hPa Φ (thick solid)
F2D (thin solid)
reflectivity (shaded)
2100UTC 12/25
2700m 2760m
12
13
Mesoscale evolution
700-hPa Φ (thick solid)
F2D (thin solid)
reflectivity (shaded)
MM50000UTC 12/26
2670m 2728m
13
14
QPF 24-h accumulated precipitation (liquid equivalent)
1200UTC 12/25 ~ 1200UTC 12/26
Max = 76mm
Max = 53mm
underpredict~ 30%
Max = 59mm
underpredict~ 22%
Max = 46mm
underpredict~ 40%
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Band life cycle
• Band formation
• Band maturity
• Band dissipation
• Model time series
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Band formation
Conv.
R1
R2
Conv.
R1*
R2*
Conv.
R2Defm.
Conv.
R2*Defm.
1802UTC WSR-88D
1929UTC WSR-88D
1800UTC MM5
1930UTC MM5
F2D (shaded)
θ (solid)
Reflectivity, 1km (shaded)
wind, 3km (barb)
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Reflectivity (shaded)
Ascent (dot)
F2D (solid)
EPV (shaded) RH=100% (thick solid)
Negative η (dot)
θes (gray solid)
II & CICI
II & CI
snowfall
F2D max
Ascent max
1802UTC WSR-88D
1800UTC MM5
II
F2D max
Ascent max
II
CI:conditional instability
II: inertial instability
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Band maturity2101UTC WSR-88D 2100UTC MM5
2100UTC MM5
R2R2*
F2D (shaded)
θ (solid)
Reflectivity, 1km (shaded)
wind, 3km (barb)
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Reflectivity (shaded)
Ascent (dot)
F2D (solid)
EPV (shaded) RH=100% (thick solid)
Negative η (dot)
θes (gray solid)
2101UTC WSR-88D
2100UTC MM5
CI
Weak CSI
II
II
F2D max
Ascent max
F2D max
Ascent maxCS
Weak CSI
CS:conditional stability
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2300UTC MM52359UTC WSR-88D
2300UTC MM5
R2
R2*
Band dissipation
F2D (shaded)
θ (solid)
Reflectivity, 1km (shaded)
wind, 3km (barb)
20
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2300UTC MM5
2359UTC WSR-88D
Reflectivity (shaded)
Ascent (dot)
F2D (solid)
EPV (shaded) RH=100% (thick solid)
Negative η (dot)
θes (gray solid)
II
CI
II
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Model time series
Cross section A-B
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Moisture availability
Obs: IPW
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Band formation (1930UTC 12/25 MM5)
Band dissipation (2200UTC 12/25 MM5)
1930UTC
2200UTC
1930UTC
2200UTC
24
2525
Compare QPF between 2100UTC and 2200UTC
Ascent profile Θe profile (QPF2200-QPF 2100)/QPF 2100
same -6%
same -23.5%
=> Changes in ascent dominated changes in moisture
MD
-0.14
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• Band evolution=> forcing, stability, and moisture
• Forcing (MM5 results)(1) Band formation deepening of a midlevel trough Increase in deformation, convergence, and frontogenesis
(2 )Band dissipation midlevel trough less defined, and frontogenesis weakened Conditional stability led to weak frontal circulation
Summary and discussion
27
Summary and discussion
• StabilityConventional thinking: CI and SI increase => band formationThis study: CI occurred before band formation~1.5h band formation: CI decrease & F2D increase
• W max & F2D maxPrevious study: W max locate on the warm side of F2D max ~50-200km This study: W max and F2D max are nearly coincident
28
Summary and discussion
• Moisturesource: Atlantic Ocean (band formation)change of ascent => change of moisture
• QPFMM5 underforecast ~30% max preci. (Δx=4km)axis of heaviest preci. ~50km to the SE of the observation locationHigher horizontal model resolution => improvement QPF much better improvement on F2D, stability, and moisture
Thanks for your listening.&
Questions?
30
Conditional instability (CI)
0
zes
0
zes
(Holton, 2004: An Introduction to Dynamic Meteorology (4 th Ed.), Fig9.10, p.294)
(2) Air parcel reach the LFC
0
zes
(1)
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Inertial instability (II)
Absolute momentum: M = fy - ug
(Holton, 2004: An Introduction to Dynamic Meteorology (4th Ed.), p.205)
In this study, set M = fy – u u=ug+u’
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Fig.7
Fig.8
Band formation
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