Dual-Polarization Operations Assessment Status Update on Development Process Progress on RDA work Progress on RPG work Where we are with Beta and Deployment.

Slides:



Advertisements
Similar presentations
POLARIMETRIC RADAR IMPROVEMENTS
Advertisements

NEXRAD or WSR-88D [Next Generation Radar] [Weather Surveillance Radar, 1988, Doppler]
7. Radar Meteorology References Battan (1973) Atlas (1989)
29 COMET Hydrometeorology 00-1 Matt Kelsch Tuesday, 19 October 1999 Radar-Derived Precipitation Part 2 I.Radar Representation of.
Page 1 Operational use of dual- polarisation: lessons learned at Météo France after 8 years of experience at all wavelengths (S / C / X) P. Tabary Météo.
MPING: Citizen Science Research Kim Elmore (NSSL/CIMMS)
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.
National Weather Association 31 st Annual Meeting 18 October 2006 Cleveland, Ohio Kevin Scharfenberg University of Oklahoma Cooperative Institute for Mesoscale.
Clear air echoes (few small insects) -12 dBZ. Echoes in clear air from insects Common is summer. Watch for echoes to expand area as sun sets and insects.
DUAL-POLARIZATION OF WSR-88D NETWORK
Radar-Derived Rainfall Estimation Presented by D.-J. Seo 1 Hydrologic Science and Modeling Branch Hydrology Laboratory National Weather Service Presented.
The WSR-88D at the National Severe Storms Laboratory, KOUN, was upgraded to add polarization diversity in KOUN transmits each EM pulse with an orientation.
Rainfall Monitioring Using Dual-polarization Radars Alexander Ryzhkov National Severe Storms Laboratory / University of Oklahoma, USA.
Rainfall Rate Relationships in WSR-88D Rainfall Estimation Algorithms Dan Berkowitz Applications Branch Radar Operations Center.
New Concepts in Utilization of Polarimetric Weather Radars Alexander Ryzhkov (CIMMS) February 25–27, 2015 National Weather Center Norman, Oklahoma.
What can Dual-Polarization Doppler Radar Do for You? Neil Fox Department of Atmospheric Science University of Missouri - Columbia.
High-Resolution X-band Dual-Polarization Weather Radar: Theory and Applications Sense and Nonsense on precipitation and drop size distribution estimation.
Using Bragg Scattering for ZDR calibration V. Melnikov (CIMMS) and D. Zrnic (NSSL) February 25–27, 2015 National Weather Center Norman, Oklahoma.
Aerosol effects on rain and hail formation and their representation using polarimetric radar signatures Eyal Ilotovich, Nir Benmoshe and Alexander Khain.
Surveillance Weather Radar 2000 AD. Weather Radar Technology- Merits in Chronological Order WSR-57 WSR-88D WSR-07PD.
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.
NEXRAD Dual-Polarization Product Review Kevin Scharfenberg OU-CIMMS and NOAA-NSSL 2 nd Workshop on NWS Severe Weather Warning Technology July 2007.
WSR‐88D Dynamic Scanning
Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy Precipitation Events Comparison of PPS and QPE Rainfall Estimates for Summer 2013 Heavy.
Similar in concept to JDOP, except with the goal to operationally demonstrate the value of the polarimetric upgrade of the 88D. Multi-seasonal to study.
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.
Introduction to the Dual-Polarized WSR-88D
WSR-88D Dual Polarization Initial Operational Capabilities WSR-88D Dual Polarization Initial Operational Capabilities 25th AMS Conference on International.
CARPE-DIEM 13/6/02, slide 1German Aerospace Center Microwaves and Radar Institute CARPE-DIEM Besprechung Helsinki, June 2004 Ewan.
Radar Basics and Estimating Precipitation Jon W. Zeitler Science and Operations Officer National Weather Service Austin/San Antonio Forecast Office Science.
Drizzle, Shallow Events Martin Hagen with the help from Elena Saltikoff, Paul Joe and others Deutsches Zentrum für Luft- und Raumfahrt (DLR) Oberpfaffenhofen,
National Weather Service Dual-Polarization Radar Technology Photo courtesy of NSSL.
Dual Polarization Technology: The KICT Upgrade Paul Schlatter Warning Decision Training Branch Paul Schlatter Warning Decision Training Branch AMS/NWA.
Dual-Pol Radar Data: A Brief Primer and A Few Brief Pseudo-Operational Exercises (Courtesy of) Dan Miller Science and Operations Officer NWS/WFO Duluth,
The Role of Polarimetric Radar for Validating Cloud Models Robert Cifelli 1, Timothy Lang 1, Stephen Nesbitt 1, S.A. Rutledge 1 S. Lang 2, and W.K. Tao.
METR February Radar Basics RADAR - acronym for RAdio Detection And Ranging; a radio device or system for locating an object by means of ultrahigh-frequency.
National Lab for Remote Sensing and Nowcasting Dual Polarization Radar and Rainfall Nowcasting by Mark Alliksaar.
Correlation Coefficient (CC)
Radar Palet e Home Dual Polarized Analysis & Diagnosis 1 Precipitation Phase – Radar Signatures Radar characteristics of precipitation types –Stratiform.
RAdio Detection And Ranging. Was originally for military use 1.Sent out electromagnetic radiation (Active) 2.Bounced off an object and returned to a listening.
1 RADAR OPERATIONS CENTER (ROC) EVALUATION OF THE WSR-88D OPEN RADAR DATA ACQUISITION (ORDA) SYSTEM SIGNAL PROCESSING WSR-88D Radar Operations Center Engineering.
Initial Implementation of Super-Resolution Data on the NEXRAD Network Dr. Sebastian Torres CIMMS/NSSL A presentation to the Data Quality Team June 15,
Reflectivity and Radial Velocity
A Two-Dimensional Velocity Dealiasing Algorithm for the WSR-88D W. Dave Zittel, Zhongqi Jing Radar Operations Center, Norman, OK Nicholas Langlieb WFO,
What to make of this new radar technology Luke Madaus, UW Atmospheric Sciences 11/2/2011.
WEATHER SIGNALS Chapter 4 (Focus is on weather signals or echoes from radar resolution volumes filled with countless discrete scatterers---rain, insects,
Quantitative Precipitation Estimation by WSR-88D Radar Dan Berkowitz Applications Branch Radar Operations Center.
WSR-88D Radar Rainfall Estimation Present and Near Future Daniel S. Berkowitz Applications Branch NWS Radar Operations Center Norman, Oklahoma 1.
Radar Palet e Home Dual Polarized Analysis & Diagnosis 1 Dual Polarized Radar What is polarimetric radar Polarimetric products Uses of these ‘raw’ outputs.
What does radar measure? Hydrometeors: rain drops, ice particles Other objects: e.g. birds, insects.
Alexander Ryzhkov Weather Radar Research Meteorological Applications of Dual-polarization Radar.
METR February Radar Products More Radar Background Precipitation Mode: -Volume Coverage Patterns (VCP) 21: 9 elevation angles with a complete.
Dual-Polarization Radars
Infilling Radar CAPPIs
National Weather Association 31 st Annual Meeting 17 October 2006 Cleveland, Ohio Kevin Scharfenberg University of Oklahoma Cooperative Institute for Mesoscale.
Radar Requirements David J. Stensrud NOAA/National Severe Storms Laboratory 2013 Warn-on-Forecast Workshop and Technical Guidance Meetings.
Dual-pol obs in NW Environment B. Dolan and S. Rutledge OLYMPEX planning meeting Seattle, 22 January 2015.
Mark Ratzer February 26 th, 2011 WFO Chicago 2 nd Annual Aviation Weather Workshop.
DUAL-POLARIZATION RADAR UPGRADE Emergency Manager Workshop Feb Chad Entremont.
Radar Interpretation Chad Entremont National Weather Service Jackson, MS.
Estimating Rainfall in Arizona - A Brief Overview of the WSR-88D Precipitation Processing Subsystem Jonathan J. Gourley National Severe Storms Laboratory.
Observations of Specific Differential Phase, KDP Chris Collier Acknowledgements: Lindsay Bennett, Alan Blyth and David Dufton.
NEXRAD Product Improvement- Update 2008 Bob Saffle: Noblis, Inc. Mike Istok: National Weather Service Greg Cate: National Weather Service AMS 24 th IIPS.
Travis Smith U. Of Oklahoma & National Severe Storms Laboratory Severe Convection and Climate Workshop 14 Mar 2013 The Multi-Year Reanalysis of Remotely.
A Moment Radar Data Emulator: The Current Progress and Future Direction Ryan M. May.
DUAL POLARIZATION AND ZDR CALIBRATION IMPROVEMENTS 5.2(6)
Presentation transcript:

Dual-Polarization Operations Assessment Status Update on Development Process Progress on RDA work Progress on RPG work Where we are with Beta and Deployment

RDA Work Data Quality Team Data Quality Team – Many, many, many problems identified, researched and fixed – Training, engineering and research experts who meet regularly Beta test will be key… Beta test will be key… – Currently Scheduled for Dec 2010 – March 2011

What Dual-Pol Does Not Change Basic WSR-88D characteristics Basic WSR-88D characteristics – Frequency, beamwidth, data resolution VCP sampling VCP sampling – Elevations, update time, number of pulses per radial All Pre-Dual-Pol products and algorithms All Pre-Dual-Pol products and algorithms You control how and when you integrate Dual-Pol information into your methodology

Dual-Pol and CMD CMD will not be operational with initial deployment CMD will not be operational with initial deployment – Manual clutter management returns! Bypass Maps for normal clutter Bypass Maps for normal clutter All Bins for AP clutter All Bins for AP clutter CMD will return with the first full build after Dual-Pol CMD will return with the first full build after Dual-Pol – Build 13…scheduled Jan/Feb 2012 – Development work underway…

Dual-Pol and Sensitivity Sensitivity: ability to detect weak returns Sensitivity: ability to detect weak returns – Measured as ___ ___ range for returned signal = noise Affected by transmitted power and system noise Affected by transmitted power and system noise – If returned signal is above the noise, life is good!

Dual-Pol Sensitivity Loss Dual-Pol radars transmit and receive both horizontally (H) and vertically (V) Dual-Pol radars transmit and receive both horizontally (H) and vertically (V) – For same range, same target, WSR-88D Dual-Pol has less returned power than before

Dual-Pol and Sensitivity Dual-Pol sensitivity loss means more gates that are “Off” than before Dual-Pol sensitivity loss means more gates that are “Off” than before –Returned signal not processed into base data Detectable Not Detectable

Dual-Pol Sensitivity Loss A bit more loss from hardware that does the splitting A bit more loss from hardware that does the splitting Cabling, built-in test equipment, etc. Cabling, built-in test equipment, etc. Per site expected sensitivity loss due to Dual-Pol conversion 3.5 – 4 dB Per site expected sensitivity loss due to Dual-Pol conversion 3.5 – 4 dB Impact on operations?!!? Impact on operations?!!?

Dual-Pol Sensitivity Loss Impact on Operations? SME panel assembled to evaluate impact of 4 dB loss SME panel assembled to evaluate impact of 4 dB loss – ROC engineering, NWS SSDs, NSSL, and WDTB Spectrum of weather events evaluated Spectrum of weather events evaluated – 4 dB loss simulated (Don’t try this at home)

Dual-Pol Sensitivity Loss Impact on Operations Events evaluated Events evaluated – Dryline – KS (KDDC) – Freezing drizzle – KS (KICT) – Marginal lake effect snow – NY (KBUF) – Tornadic supercell along boundary – CO (KFTG) – Outflow boundaries from convection – OK (KTLX) – Short range smoke plumes – OK (KTLX) – Multiple outflow boundaries/popcorn showers – FL (KEVX) – California wildfires – CA (KSOX) – Hurricane Ike landfall – TX (KHGX) – Nor’easter snowstorm (snowmaggedon) – VA (KLWX) Go Paul!! Go Paul!!

Now For Calibration of Z Calibration is about the magnitude of Z values Calibration is about the magnitude of Z values KCRI 0.5˚ KOUN 0.5˚

Calibration of Z Given appropriate Z calibration and same scatterers in a volume Given appropriate Z calibration and same scatterers in a volume –40 dBZ is 40 dBZ, 30 dBZ is 30 dBZ, etc. –Assuming Rayleigh scattering… Work is ongoing Work is ongoing –Z calibration –ZDR calibration

Sensitivity and Calibration Summary Sensitivity: more Off gates with Dual-Pol Sensitivity: more Off gates with Dual-Pol – Per site expected sensitivity loss due to Dual- Pol conversion 3.5 – 4 dB Less return from very weak signal areas Less return from very weak signal areas Z Calibration: magnitude that is assigned Z Calibration: magnitude that is assigned – Dual Pol calibration much more complex Be kind to your techs! Be kind to your techs! – 8 hour check no longer transparent

Now For Attenuation Impact on base moments does not change Impact on base moments does not change Impact on Dual-Pol products is more significant Impact on Dual-Pol products is more significant KOUN: Dual-Pol KCRI: Single Pol

Attenuation and Dual Pol Products What has happened to ZDR? What has happened to ZDR? What are the consequences? What are the consequences?

Attenuation and Dual Pol Products What has happened to CC? What has happened to CC? What are the consequences? What are the consequences?

RPG Work Dual-Pol algorithms: lots of room to grow* Dual-Pol algorithms: lots of room to grow* – Knowledge base (research) central Oklahoma – Base data from RDA only recently mature enough for RPG testing – Greatest emphasis now is QPE MLDA HCA *Been there, done that: WSR-88D original development

Quantitative Precipitation Estimation Algorithm Benefits of Dual-Pol applied to rainfall estimation Benefits of Dual-Pol applied to rainfall estimation – Dual-Pol better at identifying ground clutter, biological scatterers, large hail, etc. Prevent these returns from being converted to rainfall Prevent these returns from being converted to rainfall Legacy Precipitation Processing System and products do not go away Legacy Precipitation Processing System and products do not go away

QPE Basics QPE is an RPG algorithm QPE & PPS have similarities & differences QPE supported by other Dual-Pol algorithms – – Hydrometeor Classification Algorithm (HCA) – – Melting Layer Detection Algorithm (MLDA)

QPE Similarities With Legacy PPS Accumulations start and stop based on coverage and intensity Accumulations start and stop based on coverage and intensity – Actual start and stop times will differ

QPE Similarities With Legacy PPS Exclusion zones Exclusion zones – Prevent returns (e.g. moving clutter) from being converted to rainfall – Zones defined separately for PPS and QPE Recommend same zones initially Recommend same zones initially

QPE Similarities With Legacy PPS Storm total accumulations reset at RPG Storm total accumulations reset at RPG

QPE Similarities With Legacy PPS Concept of Hybrid Scan same Concept of Hybrid Scan same – Find lowest unblocked elevation of valid precipitable return Common accumulation periods for PPS and QPE products Common accumulation periods for PPS and QPE products – One hour, storm total, user defined

QPE Differences From Legacy PPS HCA and MLDA input used to build QPE Hybrid Scan HCA and MLDA input used to build QPE Hybrid Scan – Prevent non-meteorological returns (e.g. clutter, biological) from conversion to rain rate – Determine best rain rate computation to use

How QPE Builds Hybrid Scan Each bin gets Hydroclass value from HCA Each bin gets Hydroclass value from HCA Biological Clutter Rain Heavy Rain Ice Crystals Wet Snow Big Drops Graupel Hail-Rain Unknown Dry Snow

How QPE Builds Hybrid Scan GC (clutter), UK (unkown) GC (clutter), UK (unkown) – Go up next tilt BI (biological), no echoes BI (biological), no echoes – Don’t search higher and set rain rate to 0.0 Remaining Hydroclass values are precipitable Remaining Hydroclass values are precipitable – Lots of details on this one…some other time!

QPE Differences From Legacy PPS QPE Hybrid Scan Hydroclass R(Z) R(Z,Z DR ) R(K DP ) PPS R(Z) Hybrid Scan Reflectivity QPE rain rate product every volume scan QPE rain rate product every volume scan

Why is QPE Work Going On NOW? Base data from RDA only recently (May!) mature enough for RPG testing Base data from RDA only recently (May!) mature enough for RPG testing – But wait! There’s more! LNAs switched out in July RDA work requires frequent shutdowns RDA work requires frequent shutdowns – QPE and PPS both require High quality base data High quality base data Appropriate clutter filtering Appropriate clutter filtering RDA stable and calibrated RDA stable and calibrated

QPE is an Algorithm Base Data Rules! Base Data Rules!

QPE Work Currently Underway Attenuation and QPE Attenuation and QPE Easy to identify in base data Easy to identify in base data

QPE Work Currently Underway QPE can show zero rain rates QPE can show zero rain rates – Attenuation correction for DP variables being worked

QPE Work Currently Underway R(KDP) performance looks good so far R(KDP) performance looks good so far R(Z,ZDR) performance R(Z,ZDR) performance – Significant underestimation of high efficiency (warm rain) rainfall – Underestimation similar to R(Z) QPE Hybrid Scan Hydroclass R(Z) R(Z,Z DR ) R(K DP )

QPE Work Currently Underway R(Z,ZDR) performance R(Z,ZDR) performance Warm rain event, flash flooding in OKC Warm rain event, flash flooding in OKC – We were lucky to discover this (warm rain in OK and KOUN was running) Gage: QPE: 4.40 PPS: 4.81

QPE Work Currently Underway Current version of R(Z,ZDR) based on large group of central OK rain events Current version of R(Z,ZDR) based on large group of central OK rain events – “Individual cases may vary” Solution requirement: no operator parameter changes Solution requirement: no operator parameter changes

Thank You You are an important part of this process You are an important part of this process