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Presentation<br />

for the<br />

MPAR WG Meeting 2010-03<br />

Douglas Forsyth<br />

National Severe Storms Laboratory<br />

Chief, Radar Research & Development Division<br />

November 2010


TAP – NSSL Activities<br />

• Reviewed and Commented on LL SOW<br />

• Proceeded with TASK VI – BCI Contract<br />

– Finalize design of prototype RF and control electronics<br />

– Begin fabrication of the RF and control modules<br />

– Goal – Build 12x12 dual polarized radiating panel for<br />

operation at 3.2 GHZ.<br />

• Continued work on White-Paper Request for<br />

Proposals<br />

• Completed Evaluation on SBIR – FreEnt<br />

• Continued Risk Reduction using NWRT


Current Work – Since June 2010<br />

• Signal Processing<br />

– Continued testing adaptive range oversampling<br />

• Result of PAR DSP infrastructure improvements (ease of adding<br />

processors)<br />

• Result: Reduced scan time by factor of 2 with improved data<br />

quality.<br />

• Adaptive Scanning<br />

– Continued testing ADAPTS-II enhancements<br />

• i.e. Elevation-prioritized scanning<br />

• Scheduled base scanning<br />

– Different storms scanned with different settings and update times<br />

– Scheduler plans the best sequence of tasks to meet requested<br />

performance.<br />

– Optimizes utilization of radar resources.


Current Work – Since June 2010<br />

• Scan Processing functionality<br />

• Moved from RTC to Digital Signal Processor<br />

• Reduce computation in RTC and allow for maximum<br />

flexibility<br />

• Radar User Interface<br />

– Manual schedule-based scanning<br />

• Modify scanning strategies and change acquisition<br />

parameters on the fly<br />

• Looking at optimum ways to scan storms


Current Work – Since June 2010<br />

• Continued data analysis of NWRT Data & working on<br />

results from PARISE<br />

– Papers presented at AMS Severe Local Storms Conference<br />

• Continued work on Model Initialization with PAR data<br />

• Continued Work by OU Collaborators<br />

– Dual-Polarization element design<br />

– Eight Channel addition to the NWRT (Mono-pulse, Clutter<br />

channels)<br />

– Cylindrical Dual-Polarized PAR antenna<br />

– Mobile Imaging Radar<br />

• Wind Turbine Mitigation<br />

– Follow-on funding by DHS


Upgrades<br />

Radar<br />

Hardware<br />

Radar Control<br />

Interface<br />

(client)<br />

A/D<br />

Converters<br />

Real Time<br />

Controller<br />

Radar Control<br />

Scheduler Interface<br />

(server)<br />

Adaptive<br />

scanning<br />

Archive<br />

ATP<br />

Processor<br />

SKY Signal<br />

DSP Cluster<br />

Processor<br />

Displays<br />

Archive<br />

Data<br />

Control<br />

Original<br />

Upgraded


User Interface – Adaptive Scanning


User Interface – DSP Status


Range Oversampling


Multi- Receiver System<br />

eight downconverters<br />

eight LNA’s<br />

1 - Az Diff<br />

1 - El Diff<br />

Monopulse<br />

6 – Clutter Channels<br />

Courtesy of Mark Yeary<br />

Installed rack w/ digital receivers


MCR 1: Sum<br />

MCR 2: Delta Az<br />

MCR 3: Delta El<br />

MCR 4: Sidelobe


MCR 5: Sidelobe<br />

MCR 6: Sidelobe<br />

MCR 7: Sidelobe<br />

MCR 8: Sidelobe


MCR 1: Sum<br />

NWRT: Sum


22 nd Vaisala Award<br />

• “Rapid Sampling of Severe Storms by the<br />

NWRT Phased array Radar”<br />

– Weather & Forecasting, 2008


More Firsts for NWRT PAR<br />

031811 UTC 14 May 2009<br />

20 km 20 km<br />

KTLX<br />

KTLX<br />

PAR<br />

PAR<br />

1. First tornadic supercell sampled within 40 km of PAR<br />

- mesocyclones & other vortices within 20 km<br />

2. First supercell advantageously positioned for dual-Doppler<br />

analysis using PAR and KTLX


Did 43 s updates improve depiction of tornado<br />

cyclone evolution?<br />

PAR: 43 s Updates<br />

KTLX: 4.2 min Updates


250 m AGL, 0338:00 – 0346:15 UTC<br />

Vertical Velocity, 1 m s -1 contours<br />

Storm-relative wind vectors<br />

0335:45 UTC<br />

0338:00 UTC 0340:15 UTC 0342:30 UTC<br />

20 ms -1<br />

Vertical Vorticity, 5 x 10 -3 s -1 contours<br />

EF0 Tornado<br />

20 ms -1


Conclusions<br />

43 s updates at 0.5 provided depiction of tornado cyclone<br />

evolution superior to WSR-88D updates<br />

The amplification of vertical vorticity assoc. w/ the tornado<br />

• occurred during the occlusion phase, along axis of<br />

convergence<br />

• evolution suggests vortex co-located with updraft<br />

became dominant likely in response to vortex stretching and<br />

merging with vortex center to its south

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