PDF, 7.4 MB

More documents

Recommendations

Info

Z-R Problems• Precipitating clouds have different drop sizedistributions (DSD) requiring different Z-Requations.Z=1mm 6 m -3 Z=.25mm 6 m -3Z = 1∆V Σ 6iD iSame rainfall amount, but different reflectivities!
“Mass Flux” Impactsfrom Dotzek and Fehr (submitted to J. Appl. Metr.)• KAMM (Karlsruhe Mesoscale Model) shows theimpact of vertical velocities on rainfall ratesw=0 w=“on”
Page 1 and 2: Towards Improvements in QPEfor Flas
Page 3: Quantitative PrecipitationEstimatio
Page 7 and 8: Ground Clutter• Results from rada
Page 9 and 10: Beam Overshooting/Mixed-Phase Sampl
Page 11 and 12: And the Result is…• Overestimat
Page 13 and 14: 5. Multisensor QPEA little history
Page 15 and 16: Modules in Polar Coordinates• Rad
Page 17 and 18: AP and GC removal(Phoenix, AZ)befor
Page 19 and 20: Conv/Strat Segregation• dBZ > 50
Page 21 and 22: Bright Band Identification(BBID)•
Page 23 and 24: Comparisons of BBID withVertically-
Page 25 and 26: Radar Sampling ofPrecipitation Type
Page 27 and 28: Generate Polar Products(Text, Nids,
Page 29 and 30: CartesianModules in CartesianCoordi
Page 31 and 32: Determination of PrecipitationPhase
Page 33 and 34: Generating Multisensor FieldRegress
Page 35 and 36: QPE SUMS Product Generation• 3 di
Page 37: Evaluation Efforts• Case study ap
Page 42 and 43: CentennialWashPhoenix RadarYuma Rad
Page 44 and 45: QPESUMS Radar Only -Storm Total Pre
Page 46 and 47: Gauge Comparison:Storm Total Statis
Page 48 and 49: 6-Month Statistics in OKDomain: Bia
Page 50 and 51: MultisensorRadar-OnlyRMS Error
Page 52 and 53: Latest Improvements andDiagnostic P
Page 54 and 55:
Radar Calibration Differences
Page 56 and 57:
KIWA Hybrid ScanAfterBefore
Page 58:
Questions???gourley@ou.edu
show all

PDF, 7.4 MB

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?