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Nowcasting Flash Floods andHeavy Precipitation ---A Satellite Perspective
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Satellite Pictures
Satellite Pictures
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Hydrologic Cycle
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Quantitative Precipitation Forecasts (QPF)
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Questions to ask when preparing Nowcasts and QPF“this involves”
Global to Synoptic Scale
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Synoptic to Mesoscale
Use of Water Vapor(6.7 mm) Imagery
6.7 mm Water Vapor Plumes
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Precipitation Efficiency Factors
Precipitation Efficiency Factors
Precipitation Efficiency Factors
Additional Precipitation Efficiency Factors
Use of Precipitable Water (PW) and Relative Humidity (RH) Data
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Precipitable Water Available
Defense MeteorologicalSatellite Program/SpecialSensor Microwave Imager(SSM/I) Channel most sensitive to Total Precipitable Water22.235 GHz
GOES 8 Sounding Channels Sensitive to Precipitable Water (mm) (over land and water, cannot calculate when clouds are present) 14.37; 14.06; 13.96; 13.37; 12.66; 12:02; 11.03; 7.43; 7.02; 6.51; 4.57; 4.52; 4.13 Cloud Detection 3.74 and 0.94
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Precipitable Water X Relative Humidity
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Equivalent Potential Temperature Ridge Axis
Equivalent Potential Temperature Ridge Axis
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Short Waves(lifting mechanisms)
Short Waves(lifting mechanisms)
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Synoptic and Mesoscale BoundariesCharacteristics in the conventional data: - wind - temperature - moisture - pressureCharacteristic in the satellite data: - cloud line - moisture-dry air interface - wind
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Mesoscale to Storm scale
Interactive Flash Flood Analyzer (IFFA) Precipitation EstimatesAssign precipitation rates to the following satellite features: - Cloud top temperature and cloud growth - Mergers - Overshooting tops - Stationary Storms (speed of movement)The amount of available moisture (determined by the current Precipitable Water and Relative Humidity) is used to adjust the rainfall estimates
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NOAA/NESDIS Automatic satellite rainfall estimation .. Auto-Estimator
Resource Requirements to “Run” Flash Flood Algorithms
GOES MultiSpectral Rainfall Algorithm (GMSRA)
GOES MultiSpectral Rainfall Algorithm (GMSRA)
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Special Sensor Microwave Imager (SSM/I) (DMSP) and Advanced Microwave Sensing Unit (AMSU) (NOAA K) Precipitation EstimatesEmission - Based
SSM/I and AMSU) Precipitation EstimatesScattering Based
Special Sensor Microwave Imager (SSM/I) (DMSP) Channels Sensitive to Precipitation
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PRECIPITATION POTENTIAL(P)P = E x C VWhere E = Precipitation Estimates C = Cross-section thru stormV = Speed of storm
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How much more rain ?How much longer ?Where is the rain going to move?----------------------------------------------The answer to these questions is:“How do you expect the convection to PROPAGATE”?
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Nowcasting Flash Floods“ Look for steady state conditions that will produce congruent paths of heavy rain cells “
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