STEPS Severe Thunderstorm Electrification and Precipitation Study May-July 2000
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Transcript of STEPS Severe Thunderstorm Electrification and Precipitation Study May-July 2000
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STEPSSevere Thunderstorm
Electrification and Precipitation Study
May-July 2000
STEPSSevere Thunderstorm
Electrification and Precipitation Study
May-July 2000Prof. Steven RutledgeDepartment of Atmospheric ScienceColorado State University
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Radar NetworkRadar Network
Dual-Doppler Dual-Doppler and Tripleand TripleDopplerDopplerconfigurationsconfigurations
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STEPS Ops CenterSTEPS Ops Center
CSU-CHILL National Radar Facility; 10 cm polarimetric/DopplerCSU-CHILL National Radar Facility; 10 cm polarimetric/Dopplerwww.chill.colostate.eduwww.chill.colostate.edu
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STEPS Fixed Instrumentation: Triple-Doppler Network and LMA (VHF TOA)
STEPS Fixed Instrumentation: Triple-Doppler Network and LMA (VHF TOA)
At KGLD:At KGLD:
-NWSNWS
-T-28T-28
-NSSLNSSL
-Electric field Electric field balloonballoon
-Mobile Mobile mesonetmesonet
-MGLASSMGLASS
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Storm swath of base reflectivities (2100-0251 UTC) with NLDN lightning data overlaid.
2130 UTC2130 UTC
2328 UTC2328 UTC
0110 UTC0110 UTC
0251 UTC0251 UTC
KGLDKGLD
Tessendorf et al., JAS, 2005
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29 June Supercell• Inverted tripole• +CGs
3 June storm• Inverted dipole• No CGs
23 June storm Early: normal tripole, -CGs
Later, collapse: inverted tripole, +CGs
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29 June
3 June
23 June
Q: Why did charge structures differ?A: Supercooled liquid watercontent.
+
+
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Switching gears now, lets talk about polarimetric radar……
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NWS Polarimetric upgrade!!
NWS Polarimetric upgrade!!
A really exciting opportunityfor the science communityas well!
The STSR architecture first developed on the CSU-CHILL radar in 1995. Proof of concept.
In STSR, H-V polarizations transmitted at the same time. Previously, alternate transmission of H,V used. Needed method to switch polarizations with so called “ferrite” switch—very unreliable.
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The polarization variables..
The polarization variables..
In addition to Z and Doppler velocity..Zdr, differential reflectivity
Sensitive to particle shape and phasePower based measurement
Φdp, differential phase (Kdp)Sensitive to particle shape and phase
Phase based measurement
ρhv, correlation coefficientSensitive to particle shape and phase
Power based measurement
In addition to Z and Doppler velocity..Zdr, differential reflectivity
Sensitive to particle shape and phasePower based measurement
Φdp, differential phase (Kdp)Sensitive to particle shape and phase
Phase based measurement
ρhv, correlation coefficientSensitive to particle shape and phase
Power based measurement
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hail
rainH
V
Zdr = 10 log10 (Zhh/Zvv)
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Single particle Zdr expressed as dB
Plot from Herzegh and Jameson (1992)
Illustrates dependenceon both shape andphase, watervs. ice (dielectric)
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see Lang et al. 2004 J. Atmos. Ocean. Tech.
Non-precipitation echo: insects (preferred flight direction)
Zdr values reach CHILL data system limit (+9 dB)
Large Z and Zdr when looking at long axis of insects, orientedwith mean wind.
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Propagation Differential Phase, φdpPropagation Differential Phase, φdp
φdp is a phase based measurement, independent of power
Since the H wave encounters more dielectric compared to the V wave, the H wave moves more slowly than the V wave. H wave lags the V wave therefore in phase.
Φdp is then the phase difference (in degrees) between the H and V wave as these waves propagate out and back to the radar. This difference (degrees) will be > 0 for oblate particles (rain), zero for isotropic media (hail), and < 0 for prolate particles (e.g., oriented ice particles).
φdp is a phase based measurement, independent of power
Since the H wave encounters more dielectric compared to the V wave, the H wave moves more slowly than the V wave. H wave lags the V wave therefore in phase.
Φdp is then the phase difference (in degrees) between the H and V wave as these waves propagate out and back to the radar. This difference (degrees) will be > 0 for oblate particles (rain), zero for isotropic media (hail), and < 0 for prolate particles (e.g., oriented ice particles).
H
V
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From A. Illingworth, Chapter 5, in Weather Radar (2003)P. Meischner, Editor (Springer)
Illustration of H and V waves propagating through oblate raindrops. A phase lag between H and V waves results since the H wave moves slightly more slowly thanthe V wave, in oblate media. For prolate media, the V wave lags the H wave. Phi dp(propagation differential phase) is a measure of this phase difference between H and V waves.
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PPI display presentation of differential propagation phase
-20o diff. phase at near point
+15o ~8 km farther range
35o phase change in 8 km
Basic concept:
H, V return signal phase difference changes most rapidly in beam path segments where net differential forward scattering effects are large
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Conversion to customary Kdp units:
(Bringi and Chandra (2001) Eq 7.17)
Kdp is product of rainwater content and deviation of mass-weighted mean axis ratio from one. (Alternatively, particles with mean axis ratio of one (tumbling hailstones) do not contribute to Kdp).
Kdp is phase measurement, not dependent on accurate radar reflectivity calibration (including partial beam blockage effects), Zdr offsets / drifts, etc.
From a physical perspective….
Kdp is only arrived at after “filtering” the range profile of φdp
Too little filtering introduces noise in rain estimates, too muchfiltering removes fine scale estimates of rain rate and rain ratelocal peaks.
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Increasing rain rate
Rain rate estimation…
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CHILL: Rainfall AccumulationOptimization Algorithm
CHILL: Rainfall AccumulationNEXRAD Z-R Algorithm
Icecontamination!
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Engineering Parking Lot at Colorado State University: Flash Flood of 28 July 1997
CHILL observations of the Ft. Collinsflood led to research that caused theNWS in Denver to modify their algorithmsused to derive rainfall rates from NWS radar measurements
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An Example from the Ft. Collins Flash Flood of 28 July 1997: Cumulative Rainfall
An Example from the Ft. Collins Flash Flood of 28 July 1997: Cumulative Rainfall
Gauge Survey
Z = ARb
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Vertical structure of microphysical classification
Hydrometeor type classification results for 5 July storm from STEPS (data from CSU-CHILL)—Model Intercomparison
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Squall line and HID usingpolarimetric variables
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Co-polar H,V Correlation (ρhv)Co-polar H,V Correlation (ρhv)
The correlation coefficient is a measure of the shape variationsor irregularities in the radar resolution volume……
The correlation coefficient decreases when diverse particlestypes are present.
This diversity can be in phase of water, shape and size.
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ρhv reduction to ~0.91 in a hail shaft: 7 June 1995 near Gilcrest, CO
CSU-CHILLdata
Negative Zdr;these valuesalso modeledfor larger, wethail. Mie effectsoperate to reduce ZH relativeto ZV, leading to negative Zdr. Foraxis ratios in rangeof 0.6 to 0.8.
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hv reduced in hail area:
Mixed precip types; ρhvespecially reduced when Zrain=Zice
Diverse shapes
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Ryzhkov et al. (2005)
REMOVING NON-MET ECHO:FUZZY LOGIC CLASSIFICATION (FHC)
Clutter/AP
Rain
Insects/Birds
Example from JPOLE of rain embedded in clutter/AP and biological scatterers
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:
Primarily useful to characterize variability of scatterer characteristics within the pulse volume.
Drizzle / light rain > ~0.98
Convective (but no ice) rain > ~0.96
Hail / rain mixtures ~0.90
Bright band mixed rain and snow ~0.75
Tornado debris ~0.50 or less
Ground clutter ~0.6-0.8
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Some winter storm applications…….
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Bright band descendingto surface in rain/snowtransition
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Vertical profile in asnowstorm.
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Dual offset antenna: 2008Prof. Bringi leads a successful >$1MMRI proposal to acquire a new antenna
Offset feed design, first time be used on an S-band weather radar
Unprecedented performance has nowbeen demonstrated
Advances the Facility to a new level ofperformance
The new antenna set the stage for another major development…..
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Dual-wavelength projectDual-wavelength project No other radar like
this in the world Will allow CHILL
to make impact on NWS gap-filling radar concept
Takes advantage of CASA second generation radar
Unique dual-frequency combination enables new science
CSU cost share dollars used to acquire critical components
Will be tested later in the spring….
No other radar like this in the world
Will allow CHILL to make impact on NWS gap-filling radar concept
Takes advantage of CASA second generation radar
Unique dual-frequency combination enables new science
CSU cost share dollars used to acquire critical components
Will be tested later in the spring….12/9/2010
Main Reflecto
r
Sub-Reflector
Feed Horn
CASA Magnetron
T/R Pkg
Dual-frequencyFeed Horn
CSU-CHILL Update 36