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Echo Tops PowerPoint Presentation

Echo Tops

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Echo Tops

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  1. Echo Tops Fairly accurate at depicting height of storm tops Inaccurate data close to radar because there is no beam angle high enough to see tops. Often has stair-stepped appearance due to uneven sampling of data between elevation scans.

  2. Precipitation Estimates Storm TotalPrecipitation • Total estimated accumulation for a set amount of time. • Resets storm total whenever there is no rain detected for an hour.

  3. One Hour Precipitation Total • -Updated once per volume scan. • Shows accumulated rainfall for the last hour. • Useful for determining rainfall rate of ongoing convection.

  4. Precipitation Estimate Advantages and Limitations • Great for scattered areas of rain where no rain gauges are located • Provides a graphical ‘map’ of rainfall for an entire region • Data can be overlaid with terrain and watersheds to predict reservoir and waterway crests • Estimates based on cloud water levels and not ground level rainfall • ‘Hail Contamination’ causes highly inflated values • High terrain causes underestimates • Useful as a supplement, not replacement for ground truth information

  5. Interpreting Doppler Signatures Display examples provided by: National Weather Service Steve Davis - Lead Forecaster Milwaukee/Sullivan National Weather Service Forecast Office

  6. Azimuth Resolution Considerations • closer a rotation the more likely it will be identified correctly • rotation smaller than the 0.50 beam width (possible at long ranges) • > rotation is average of all velocities in sample volume • Previous 10 beam width improved by super-resolution Enlarged image along a radial. Individual “blocks” represent one sample volume. This graphically shows the radar resolution. Azimuth 3 Weak inbound, weak outbound Rotation too small to be resolved Azimuth 2 Strong inbound, strong outbound Azimuth 1 Rotational couplet identification can be affected by azimuth resolution. Stronger inbound than outbound

  7. The Zero Isodop “Problem” When the radial is perpendicular to wind direction, the radar displays zero velocity - This “zero zone” is called the “Zero Isodop”. What percentage of actual wind will the radar detect? 00 = 100% - Parallel 150 = 97% 300 = 87% 450 = 71% 600 = 50% 750 = 26% 900 = 0% - Perpendicular When the wind velocity is parallel to the radial, the full component of the wind is measured

  8. Large Scale Winds Use the Zero Isodop to assess the vertical wind profile. The combination shape of the zero isodop indicates both veering and backing winds with height. Combination Backward “S” Shape Backward “S” shape of the zero isodop indicates backing winds with height. Backing may imply cold air advection. “S” Shape “S” shape of the zero isodop indicates veering winds with height. Veering may imply warm air advection.

  9. Large Scale Winds Uniform Flow Straight Zero Isodop indicates uniform direction at all levels. Uniform Flow with Jet Core Straight Zero Isodop indicates uniform direction at all levels >> inbound/outbound max’s show a jet core aloft with weaker winds above and below.

  10. Example from KMKX 88D Low level jet max January 5, 1994 Steady snowfall

  11. The VAD Wind Profile(Velocity Azimuth Display)

  12. Small Scale Winds- Diffluence/Confluence - Diffluence Often seen at storm top level or near the ground at close range to a pulse type storm Confluence would show colors reversed

  13. Small Scale Winds- Cyclonic Confluence/Diffluence - Anticyclonic confluence/ diffluence would show colors reversed in each panel. Cyclonic Confluence Cyclonic Diffluence

  14. Small Scale Winds- Pure Cyclonic Rotation - Anticyclonic rotation would show colors reversed Pure Cyclonic Rotation

  15. Small Scale Velocity Example

  16. Small Scale Velocity Example Rotation with tornado

  17. Storm Relative Velocity - SRVvsBase Velocity SRV: Subtract estimated velocity of thunderstorm from the Doppler radial velocity– Make the storm stationary When diagnosing rotational characteristics, use SRV motion of the storm masks subtle rotations within the storm When diagnosing Straight Line Winds (bow echo, microbursts), use Base Velocity straight line winds are sum of the winds produced by the storms, plus storms movement

  18. SRV vs. Base Velocity- strong rotation - Storm Relative Velocity Base Velocity rotation in tornadic thunderstorm

  19. SRV vs Base Velocity- subtle rotation - Base Velocity Storm Relative Velocity Janesville F2 tornado. June 25th, 1998 ~ 700 PM Interesting note: These scans are at 3.40 elevation. The 0.50 elevation showed little rotational information.

  20. SRV vs Base Velocity- subtle rotation - 3.40 Little/no rotation seen at lowest elevation Base Velocity Storm Relative 0.50

  21. SRV vs Base Velocity Base Velocity Storm Relative Velocity

  22. SRV vs Base Velocity- straight line winds - Base velocity shows max inbound winds of 55 to 60 kts. SRV shows max inbound winds of 30 to 40 kts.

  23. Bow Echoes Detecting and Predicting Downbursts • Bow echoes are caused by severe downbursts, accelerating part of a line of thunderstorms ahead of the rest. • The strongest downbursts occur under and just north of the apex of the bow, but can occur elsewhere too • Surface winds can exceed 70mph in strong bow echoes. • Bow echoes can move at over 50 mph. • Highest reflectivities and strongest velocities are found at the apex. • Look for a tight gradient of reflectivity.

  24. Review Clear-Air Radar

  25. UHF 10 cm VHF

  26. 10 cm VHF UHF

  27. Clear-Air Wind Profilers

  28. Wind Profiler Specifications