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December 09, 2002: Light Stratiform Precipitation with embedded Non-meteorological Scatterers

Author: Pam Heinselman, CIMMS/OU

Last Updated: 9 April 2003

Forecast/Weather:

Radar Operations:

Radar/Operational Status:

Operational Delivery:

Snapshots:Two examples of non-meteorological scatterers embedded in stratiform echo (Figs. 1-4, 5-8)

Reflectivity
Figure 1: The radar reflectivity image at 18:50 UTC 9 December 2002 indicates light stratiform precipitation over central Oklahoma, but no non-meteorological scatterers.
Differential Reflectivity
Figure 2: Areas of high differential reflectivity are embedded in precipitation signal southwest and southeast of KOUN at 18:50 UTC 9 December 2002.
Correlation Coefficient
Figure 3: Correlation coefficients colocated with areas of high differential reflectivity range from 0.7 - 0.93, values which *may* indicate with chaff.
Hydrometeor Classification
Figure 4: The hydrometeor classification algorithm identifies non-meteorological scatterers as snow at 18:50 UTC 9 December 2002.
Reflectivity
Figure 5: The radar reflectivity image at 22:59 UTC 9 December 2002 indicates light stratiform precipitation over central Oklahoma, but no non-meteorological scatterers.
Differential Reflectivity
Figure 6: An area of high differential reflectivity 75-100 km south-southeast of KOUN indicates non-meteorological scatterers at 22:59 UTC 9 December 2002.
Correlation Coefficient
Figure 7: Correlation coefficients colocated with the area of high differential reflectivity south-southeast of KOUN range from 0.7 - 0.93, values which may indicate chaff.
Hydrometeor Classification
Figure 8: The hydrometeor classification algorithm identifies non-meteorological scatterers as a mix of stratiform precipitaiton and biological scatterers at 22:59 UTC 9 December 2002.