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What else is lightning used for?• Accumulations of flash density and % positive 5-m, 1-h, 24-h
Bright Band Identification(BBID)• 3-D Reflectivity Field• ID Layer of Higher Reflectivity• Vertical Reflectivity Gradient• Spatial/Temporal SmoothingPolar
Page 1 and 2: Towards Improvements in QPEfor Flas
Page 3 and 4: Quantitative PrecipitationEstimatio
Page 5 and 6: “Mass Flux” Impactsfrom Dotzek
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: Conv/Strat Segregation• dBZ > 50
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

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