X-band Mobile Radar Data Update

Slides:



Advertisements
Similar presentations
Radar/lidar observations of boundary layer clouds
Advertisements

Robin Hogan A variational scheme for retrieving rainfall rate and hail intensity.
Upper-limit on Sco X-1 S2 preliminary results C Messenger, V Re and A Vecchio on behalf of PULG LSC General Meeting LHO, 10 th – 13 th November 2003.
7. Radar Meteorology References Battan (1973) Atlas (1989)
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.
ATS 351 Lecture 9 Radar. Radio Waves Electromagnetic Waves Consist of an electric field and a magnetic field Polarization: describes the orientation.
X-band About the CSU-CHILL Radar The CSU-CHILL National Weather Radar Facility, located in Greeley, CO, is an advanced, transportable dual-polarized, dual-wavelength.
Contributors to Measurement Errors (Chap. 7) *1) Widespread spatial distribution of scatterers (range ambiguities) *2) Large velocity distribution (velocity.
The use of radar data to improve rainfall estimation across the Tennessee River Valley Transitioning from the rain gauge Patrick N. Gatlin, W. Petersen,
THE USE OF DUAL-POLARIMETRIC RADAR DATA TO IMPROVE RAINFALL ESTIMATION ACROSS THE TENNESSEE RIVER VALLEY W.A. Petersen NASA – Marshall Space Flight Center,
W EATHER R ADAR FOR URBAN PLUVIAL FLOOD FORECASTING Professor Chris Collier National Centre for Atmospheric Science, Head of Strategic Partnerships University.
Excess phase computation S. Casotto, A. Nardo, P. Zoccarato, M. Bardella CISAS, University of Padova.
Robin Hogan Anthony Illingworth Marion Mittermaier Ice water content from radar reflectivity factor and temperature.
Cabo Guasave S-Pol NAME Radar Data - Product Description & Quality Control.
RADAR EXAMPLES Images from Sandra Yuter, NCSU Frederic Fabry, McGill University Weatherworld 2010, University of Illinois Robin Hogan, University of Reading.
Developments in Radar Refractivity Retrieval John Nicol 1, Anthony Illingworth 1, Kim Bartholomew 1, Tim Darlington 2 Malcolm Kitchen 2, Jon Eastment 3.
What can Dual-Polarization Doppler Radar Do for You? Neil Fox Department of Atmospheric Science University of Missouri - Columbia.
Applicability and limitations of redundancy cal. in phased array stations Parisa Noorishad, Stefan Wijnholds, Arnold van Ardenne & Thijs van der Hulst.
Radar: Acronym for Radio Detection and Ranging
Using Bragg Scattering for ZDR calibration V. Melnikov (CIMMS) and D. Zrnic (NSSL) February 25–27, 2015 National Weather Center Norman, Oklahoma.
Doppler Radar From Josh Wurman Radar Meteorology M. D. Eastin.
Spaceborne Radar for Snowfall Measurements
Topographic Radar Beam Blockage and its Effects on Radar Rainfall Estimates: The BREAM Model Timothy A. Coleman Atmospheric Science Department The University.
Results of the WMO Laboratory Intercomparison of rainfall intensity gauges Luca G. Lanza University of Genoa WMO (Project Leader) DIAM UNIGE September.
Dual Polarization Martin Hagen, Elena Saltikoff Deutsches Zentrum für Luft- und Raumfahrt (DLR) Oberpfaffenhofen, Germany Finnish Meteorological Institute.
Radar Polarimetric Retrievals. Anthony Illingworth University of Reading, UK.
Polarization at IRAM Status and Plans S.Guilloteau Laboratoire d’Astrophysique de Bordeaux.
CARPE-DIEM 13/6/02, slide 1German Aerospace Center Microwaves and Radar Institute CARPE-DIEM Besprechung Helsinki, June 2004 Ewan.
National Weather Service Dual-Polarization Radar Technology Photo courtesy of NSSL.
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,
ELECTRONIC INSTRUMENTATION & PLC DKT Signal Conditioning Circuits.
Cavity BPM processing and hardware upgrade plans A. Lyapin, S. Boogert, E. Yamakawa.
ANSS/NSMP STRONG- MOTION RECORD PROCESSING AND PROCEDURES Christopher D. Stephens and David M. Boore US Geological Survey Menlo Park, CA COSMOS/NSF International.
The new DWD polarimetric weather radar network: a new radar data processing framework and new products Michael Frech 1, Nils Rathmann 2, Jörg Steinert.
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
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.
SRS Data Examples A brief overview of some types of radio emissions observed on the Solar Radio Spectrograph.
Dual-Polarization and Dual-Wavelength Radar Measurements Vivek National Center for Atmospheric Research Boulder, Colorado I.Polarization and dual- wavelength.
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.
DYNAMO radar workshop University of Washington, Seattle August 2012 Mike Dixon, Bob Rilling, Scott Ellis, John Hubbert and Scot Loehrer Earth Observing.
Comparison of Polarimetric C Band Doppler Radar Observations with Reflectivity Fields obtained at S Band: A Case Study of Water induced Attenuation R.
RADAR METEOROLOGY Courtney Schumacher Texas A&M University ATMO 352.
Dual-pol obs in NW Environment B. Dolan and S. Rutledge OLYMPEX planning meeting Seattle, 22 January 2015.
Use of the Moon as a calibration reference for NPP VIIRS Frederick S. Patt, Robert E. Eplee, Robert A. Barnes, Gerhard Meister(*) and James J. Butler NASA.
Status of S-PolKa Data Sets Bob Rilling, Mike Dixon, Scott Ellis, John Hubbert and Scot Loehrer EOL, NCAR, Boulder, CO DYNAMO radar workshop University.
Solid State Driver Upgrade Update 1kW Solid State Amplifiers – 32 have been tested and calibrated. – 50 have been built so far. Small heat sinks for the.
Level 1.5 Processing Updates Martin Bates, RAL GIST th April, 2005.
BASIC INSTRUMENTS - oscilloscopes
DUAL-POLARIZATION RADAR UPGRADE Emergency Manager Workshop Feb Chad Entremont.
Wireless Charging of Mobile Phones Using Microwaves
30GHz system improvements Jan Kovermann RF meeting
Observations of Specific Differential Phase, KDP Chris Collier Acknowledgements: Lindsay Bennett, Alan Blyth and David Dufton.
Statistical Analysis of S-Pol Polarimetric Radar Data from NAME 2004 Timothy J. Lang, Robert Cifelli, Steven A. Rutledge, Angela Rowe, and Lee Nelson Colorado.
SIGNAL CONDITIONING Signal conditioning is stage of instrumentation system used for modifying the transduced signal into a usable format for the final.
Karen Kosiba, Josh Wurman, Stacy Brodzik, Andrew Frambach
DUAL POLARIZATION AND ZDR CALIBRATION IMPROVEMENTS 5.2(6)
31 May UTC meeting John Hubbert and Angela Rowe
NPOL Olympex Located N/ W, 157 m ASL
3-coordinate Coastal Radar with Multi-beam Active Phased Array
Development of Assimilation Methods for Polarimetric Radar Data
Planning Spectral Observations
Giant Raindrops in mid-latitude Cumuli
Polarimetric radar analysis of convection in the complex topography
S-Pol Radar Deployment
NanoBPM Status and Multibunch Mark Slater, Cambridge University
UVIS Calibration Update
UVIS Calibration Update
Spaceborne Radar for Snowfall Measurements
Presentation transcript:

X-band Mobile Radar Data Update Lindsay Bennett and John Nicol

Z Calibration Self-consistency check using Z, ZDR and KDP (Gourley et al. 2009, JTech) Very stringent conditions to avoid effects of attenuation at X-band (i.e. 4-6 degrees of differential phase shift over 10-15 km of light rain) Only suitable data on 17th August (IOP 17) Two half-hour periods indicate a calibration offset of +4.75 dB

ZDR Calibration Based on returns at low elevation angles in light rain, a large ZDR drift during the first two hours of operation was often observed E.g. a ZDR drift of 1.2 dB (from +2.6 to +1.4 dB) on 14th and 17th August Typical ZDR calibration offset = +1.2 dB (+0.2 dB due to small oblate drops)

2-hour drift SELEX identified a problem with the STALO control cable Missing electrical bridge within one connector Prevented the STALO from changing frequency Highlighted an important sensitivity, primarily affecting ZDR during the first two of operations related to frequency drifts of the Magnetron transmitter After above repair and redesign of the IF filters, SELEX have demonstrated only a small residual effect on ZDR during the first hour of operation (still under investigation)

Analysis of strong clutter targets Returns from strong clutter targets confirms the ZDR drifts observed in light rain and its association with frequency drifts Also highlighted dBZ calibration jumps of ~1 dB affecting occasional scans on isolated occasions seem to be associated with the automated routine to measure background noise levels Only occurs on a couple of days Cause still under investigation…

Summary Overall dBZ/ZDR calibration corrections have been determined: -4.75 dB /-1.2dB Additional drift affecting ZDR in the first 2 hours of operation identified and associated with frequency changes. frequency changes were recorded and will be used to correct these effects Calibration corrections are to be applied to the entire data set in the next few months for overall offsets and ZDR drifts. A correction for dual-PRF velocity de-aliasing errors has been tested and will be implemented, improving the quality of Doppler velocity measurements Sporadic calibration jumps have been identified on a few occasions and are still to be investigated. Data from a few problem days may be withheld until the source of the calibration jumps has been determined.