Technical Interchange Meeting – ROC / NSSL / NCAR ROC / NSSL / NCAR TIM Boulder CO 11 May 2005 Real-time time-series implementation of the Radar Echo Classifier.

Slides:



Advertisements
Similar presentations
Keith Brewster Radar Assimilation Workshop National Weather Center 18-Oct-2011.
Advertisements

CLEAN-AP Update Cl utter E nvironment An alysis using A daptive P rocessing Sebastián Torres and David Warde CIMMS/The University of Oklahoma and National.
Target Separation and Classification using Cloud Radar Doppler-Spectra Matthias Bauer-Pfundstein, METEK GmbH Ulrich Görsdorf, Meteorologisches Observatorium.
1 Sebastian Torres NEXRAD Range-Velocity Ambiguity Mitigation Staggered PRT and Phase Coding Algorithms on the KOUN Research Radar.
CLUTTER MITIGATION DECISION (CMD) THEORY AND PROBLEM DIAGNOSIS
Water vapor estimates using simultaneous S and Ka band radar measurements Scott Ellis, Jothiram Vivekanandan NCAR, Boulder CO, USA.
NEXRAD TAC Norman, OK March 21-22, 2006 Clutter Mitigation Decision (CMD) system Status and Demonstration Studies Mike Dixon, Cathy Kessinger, and John.
21 September th Southwest Hydrometeorology Symposium, Tucson, AZ Future QPE: Dual-Pol and Gap-Filler Radars Kevin Scharfenberg University of Oklahoma/CIMMS.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Semester 2 Update Joe Hoatam Josh Merritt Aaron Nielsen.
Evolution of the SZ-2 Algorithm Sebastian Torres CIMMS/NSSL Technical Interchange Meeting Fall 2006.
Radar-Derived Rainfall Estimation Presented by D.-J. Seo 1 Hydrologic Science and Modeling Branch Hydrology Laboratory National Weather Service Presented.
Updates to the SZ-2 Algorithm Sebastián Torres CIMMS/NSSL Technical Interchange Meeting Fall 2007.
 Definition of Spectrum Width (σ v ) › Spectrum width is a measure of the velocity dispersion within a sample volume or a measure of the variability.
Staggered PRT Update Part I Sebastián Torres and David Warde CIMMS/The University of Oklahoma and National Severe Storms Laboratory/NOAA NEXRAD TAC Norman,
Carlos A. Rodríguez Rivera Mentor: Dr. Robert Palmer Carlos A. Rodríguez Rivera Mentor: Dr. Robert Palmer Is Spectral Processing Important for Future WSR-88D.
Cabo Guasave S-Pol NAME Radar Data - Product Description & Quality Control.
Dual-Doppler Wind Retrieval from two operational Doppler radars Yong Kheng Goh, Anthony Holt University of Essex, U. K. for ERAD04, Visby.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Dual Polarization Radar Signal Processing Dr. Chandra Joe Hoatam Josh Merritt.
Lessons learned in field studies about weather radar observations in the western US and other mountainous regions Socorro Medina and Robert Houze Department.
COPS-GOP-WS3 Hohenheim 2006_04_10 Micro- Rain- Radar Local Area Weather Radar Cloud Radar Meteorological Institute University Hamburg Gerhard Peters.
RHB C-band radar scan strategy constraints Cloud top height less than 1.5 km altitude Features of interest < 5 km in scale Rapid evolution of cells  fast.
Institut für Physik der Atmosphäre POLDIRAD Polarization Diversity Doppler Radar Martin Hagen DLR Oberpfaffenhofen.
Dual-Doppler Wind Retrieval from two operational Doppler radars Yong Kheng Goh, Anthony Holt University of Essex, U. K. for CARPE DIEM, Bologna 29 Nov.
Surveillance Weather Radar 2000 AD. Weather Radar Technology- Merits in Chronological Order WSR-57 WSR-88D WSR-07PD.
Spaceborne Weather Radar
Basic RADAR Principles Prof. Sandra Cruz-Pol, Ph.D. Electrical and Computer Engineering UPRM.
Data Windowing in ORDA Technical Briefing Sebastián Torres 1,2, Chris Curtis 1,2, Rodger Brown 2, and Michael Jain 2 1 Cooperative Institute for Mesoscale.
11/18/02Technical Interchange Meeting Progress in FY-02 Research RDA –Capability to collect time series data –Control of phase shifter Phase coding –Sigmet’s.
Sebastián Torres Weather Radar Research Innovative Techniques to Improve Weather Observations.
Sebastian Torres NEXRAD Range-Velocity Ambiguity Mitigation Spring 2004 – Technical Interchange Meeting.
Radar based Quantitative Precipitation Estimation in WRC Jae-Kyoung Lee
A Doppler Radar Emulator and its Application to the Detection of Tornadic Signatures Ryan M. May.
Oct. 12, National Severe Storms Laboratory & University of Oklahoma Information briefing to the NEXRAD Technical Advisory.
Dual-Polarization Operations Assessment Status Update on Development Process Progress on RDA work Progress on RPG work Where we are with Beta and Deployment.
LROSE – L IDAR R ADAR O PEN S OFTWARE E NVIRONMENT Mike Dixon, Wen-Chau Lee, Mike Daniels, Charlie Martin, Steve Cohn, Bill Brown Earth Observing Laboratory,
TITAN - identifying and tracking convective storms as objects 1 Heuristic Probabilistic Forecasting Workshop Munich, Germany August 2014 Mike Dixon.
Technical Interchange Meeting Spring 2008: Status and Accomplishments.
Radar Quality Control and Quantitative Precipitation Estimation Intercomparison Project Status Paul Joe Environment Canada Commission of Instruments, Methods.
Radar Palet e Home Dual Polarized Analysis & Diagnosis 1 Precipitation Phase – Radar Signatures Radar characteristics of precipitation types –Stratiform.
Chad Entremont Daniel Lamb NWS Jackson, MS
1 RADAR OPERATIONS CENTER (ROC) EVALUATION OF THE WSR-88D OPEN RADAR DATA ACQUISITION (ORDA) SYSTEM SIGNAL PROCESSING WSR-88D Radar Operations Center Engineering.
Dual-Polarization and Dual-Wavelength Radar Measurements Vivek National Center for Atmospheric Research Boulder, Colorado I.Polarization and dual- wavelength.
SuperDARN operations Pasha Ponomarenko.
Updates to the SZ-2 Algorithm Sebastian Torres CIMMS/NSSL Technical Interchange Meeting Spring 2007.
NEXRAD TAC Meeting August 22-24, 2000 Norman, OK AP Clutter Mitigation Scheme Cathy Kessinger Scott Ellis Joseph VanAndel
What to make of this new radar technology Luke Madaus, UW Atmospheric Sciences 11/2/2011.
III) CHARACTERISTICS OF THE ADDED CLUTTER RAIN MeteoSvizzera, 6605 Locarno, Switzerland Simulation.
WEATHER SIGNALS Chapter 4 (Focus is on weather signals or echoes from radar resolution volumes filled with countless discrete scatterers---rain, insects,
1 Spectral identification & suppression of ground clutter contributions for phased array radar Spectral identification of ground clutter Spectral identification.
DYNAMO radar workshop University of Washington, Seattle August 2012 Mike Dixon, Bob Rilling, Scott Ellis, John Hubbert and Scot Loehrer Earth Observing.
Sebastian Torres NEXRAD Range-Velocity Ambiguity Mitigation Fall 2004 – Technical Interchange Meeting.
Quantitative Precipitation Estimation by WSR-88D Radar Dan Berkowitz Applications Branch Radar Operations Center.
Developments in echo tracking - enhancing TITAN
Tele-Conference with Lincoln Labs: Icing Hazard Level National Center for Atmospheric Research 29 April 2010.
Alexander Ryzhkov Weather Radar Research Meteorological Applications of Dual-polarization Radar.
NCAR Activity Update John Hubbert, Cathy Kessinger, Mike Dixon, Scott Ellis, Greg Meymaris and Frank Pratte To the NEXRAD TAC October 2005 San Diego,
NEXRAD Data Quality 25 August 2000 Briefing Boulder, CO Cathy Kessinger Scott Ellis Joe VanAndel Don Ferraro Jeff Keeler.
Target Separation and Classification using Cloud Radar Doppler-Spectra Matthias Bauer-Pfundstein, METEK GmbH Ulrich Görsdorf, Meteorologisches Observatorium.
DUAL-POLARIZATION RADAR UPGRADE Emergency Manager Workshop Feb Chad Entremont.
Accuracy of Wind Fields in Convective
DUAL POLARIZATION AND ZDR CALIBRATION IMPROVEMENTS 5.2(6)
CAPS Radar QC and Remapping
NPOL Olympex Located N/ W, 157 m ASL
A dual-polarization QPE method based on the NCAR Particle ID algorithm Description and preliminary results Michael J. Dixon1, J. W. Wilson1, T. M. Weckwerth1,
NEXRAD Data Quality Optimization AP Clutter Mitigation Scheme
High resolution radar data and products over the Continental United States National Severe Storms Laboratory Norman OK, USA.
the University of Oklahoma
An overview of real-time radar data handling and compression
Examples of spectral fields
Spaceborne Radar for Snowfall Measurements
Presentation transcript:

Technical Interchange Meeting – ROC / NSSL / NCAR ROC / NSSL / NCAR TIM Boulder CO 11 May 2005 Real-time time-series implementation of the Radar Echo Classifier (REC) for clutter detection in ORDA Mike Dixon NCAR

Goal The goal was to develop and test a version of the REC with the following properties: Fast and efficient for real-time operation, suitable for use in the ORDA. Works with time series data, so that the algorithm has access to the spectral domain. Is suitable for detecting clutter and AP.

Beam processing sequence Beam 1Beam 2Beam3Beam 4Beam 5 IN Out Beam Queue Compute Moments Compute REC Filter Clutter Filtered Moments out

REC for clutter or AP detection Kernel: 5 deg wide, 2 km along the beam. Uses the following fields: –TDBZ - DBZ texture: squared change in dBZ from one gate to the next, in range, averaged over the kernel. –SPIN - DBZ ‘spin’: measure of how frequently the trend in reflectivity along a beam changes with range. Averaged over the kernel. –VEL: velocity at the gate. –SDVE: standard deviation of velocity over the kernel. –WIDTH: spectrum width at the gate. –CLUTPROB: clutter probability, based on ratios of power near 0 m/s to power in rest of spectrum.

Membership functions TDBZ SPIN WIDTH SDVE 0 1 VEL CLUTPROB 0 1

Data sets This implementation of the REC was developed to handle time-series data in LIRP format. It was tested on the following data sets: KJIM, stratiform situation, non-phase-coded. SPOL at Boulder, convective situation, phase-coded. SPOL at NAME, Mexico, convective situation, non-phase-coded, alternating-pulse dual-polarization.

KJIM Case Non-phase-coded data Stratiform rain to NW Ground clutter

KJIM dBZ

KJIM Vel

KJIM WIDTH

KJIM TDBZ

KJIM SPIN

KJIM SDVE

KJIM Clutter Probability

KJIM REC

KJIM Clutter Flag

KJIM dBZ

KJIM dBZ filtered

KJIM VEL

KJIM VEL filtered

KJIM WIDTH

KJIM WIDTH filtered

KJIM filter everywhere

KJIM dBZ

KJIM dBZ filtered everywhere

KJIM vel

KJIM vel filtered everywhere

SZ Case - SPOL SZ864 decoding Strong mountain ground clutter Convective weather situation

SZ dBZ

SZ VEL

SZ WIDTH

SZ Trip flags

SZ TDBZ

SZ SPIN

SZ SDVE

SZ REC

SZ REC Clutter Flag

SZ Clutter found

SZ dBZ

SZ dBZ filtered

SZ VEL

SZ VEL filtered

SZ WIDTH

SZ WIDTH filtered

Dual Polarization Case – SPOL at NAME Alternate-pulse dual polarization Strong ground clutter Some sea clutter at times Convective weather situation

Additional REC fields for Dual Pol The following fields were added to the REC for the dual polarization case: –RHOHV – value at the gate. –SD-ZDR – standard deviation of ZDR in range, computed for the single beam only, no azimuth averaging. –SD-RHOHV – standard deviation of RHOHV in range, computed for the single beam only, no azimuth averaging.

Membership functions – Dual Pol RHOHV SD-ZDR SD-RHOHV

Dual-pol dBZ

Dual-pol VEL

Dual-pol WIDTH

Dual-pol TDBZ

Dual-pol SPIN

Dual-pol SDVE

Dual-pol ZDR

Dual-pol SDZDR

Dual-pol RHOHV

Dual-pol SD-RHOHV

REC – no dual-pol fields

REC with dual pol fields

REC FLAG – no dual-pol fields

REC FLAG with dual pol fields

Dual-pol Clutter found

Dual-pol dBZ

Dual-pol dBZ filtered

Dual-pol VEL

Dual-pol Vel filtered

Dual-pol WIDTH

Dual-pol WIDTH filtered

Relative performance considerations Some tests were carried out on the computer time taken by the REC and clutter filtering as compared to moments estimation. The following table shows the number of seconds taken to compute moments, REC and filter clutter for a single PPI for each of the cases. The test machine was a 2.8GHz Pentium IV. These numbers are useful to show the relative costs of each operation. KJIM, filter only where REC > thresh KJIM, filter clutter everywhere SZ, filter only where REC > thresh Dual Pol, filter only where REC > thresh Moments estimation REC computation Clutter filtering

Further work Clutter filtering – handling residual power. SZ clutter filtering. Tuning the REC for dual polarization data. Pattern matching for spectra in range (NESPA, NIMA). Thank you