Zdr for chosen spectral coefficients in 5-7-2004, clear-air, day time, south wind, insects, clutter. S.Bachmann.

Slides:



Advertisements
Similar presentations
7. Radar Meteorology References Battan (1973) Atlas (1989)
Advertisements

ATS 351 Lecture 9 Radar. Radio Waves Electromagnetic Waves Consist of an electric field and a magnetic field Polarization: describes the orientation.
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.
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.
Birds, Insects, and Refractive Index Gradients as the Source of Clear-Air Return for Meteorological Radars William Martin November 9, 2005.
Rainfall Monitioring Using Dual-polarization Radars Alexander Ryzhkov National Severe Storms Laboratory / University of Oklahoma, USA.
Size Sorting in Bulk & Bin Models Onset of precip – development of particles large enough to sediment relative to cloud droplets & ice crystals. Larger.
Cabo Guasave S-Pol NAME Radar Data - Product Description & Quality Control.
Anomalous Propagation Greater density slows the waves more. Less dense air does not slow the waves as much. Since density normally decreases with height,
Günther Haase Tomas Landelius Daniel Michelson Generation of superobservations (WP2)
Copyright © 2009 Pearson Education, Inc. Lecture 4 Circular Motion 1.
What can Dual-Polarization Doppler Radar Do for You? Neil Fox Department of Atmospheric Science University of Missouri - Columbia.
Using Bragg Scattering for ZDR calibration V. Melnikov (CIMMS) and D. Zrnic (NSSL) February 25–27, 2015 National Weather Center Norman, Oklahoma.
Surveillance Weather Radar 2000 AD. Weather Radar Technology- Merits in Chronological Order WSR-57 WSR-88D WSR-07PD.
Correct atmospheric optics modelling: Theory and Experiment Irina Melnikova Observatory of Environmental Safety Resource Center, Research Park St.Petersburg.
Review Doppler Radar (Fig. 3.1) A simplified block diagram 10/29-11/11/2013METR
slide 1 German Aerospace CenterMicrowaves and Radar Institute Extraction of clear-air wind Dr. Thomas Börner DLR Oberpfaffenhofen.
Radar equation review 1/19/10. Radar eq (Rayleigh scatter) The only variable is h, the pulse length Most radars have a range of h values. Rewrite the.
Topographic Radar Beam Blockage and its Effects on Radar Rainfall Estimates: The BREAM Model Timothy A. Coleman Atmospheric Science Department The University.
Wind Profiler Signal & Data Processing -Anil Anant Kulkarni SAMEER, IIT Campus,Powai Mumbai
Phased Array Radar Configurations for Ground-Based and Airborne Deployments Dual Use: Deployable on airborne and ground-based platforms Key measurements:
Dual Polarization Martin Hagen, Elena Saltikoff Deutsches Zentrum für Luft- und Raumfahrt (DLR) Oberpfaffenhofen, Germany Finnish Meteorological Institute.
Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Polarization I: Radar concepts and ZDR part I. Dual polarization radars can estimate several return signal properties beyond those available from conventional,
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.
Study Design and Summary Atmospheric boundary layer (ABL) observations were conducted in Sapporo, Japan from April 2005 to July Three-dimensional.
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,
Basic Principles of Doppler Radar Elena Saltikoff Alessandro Chiariello Finnish Meteorological Institute.
Technical Interchange Meeting Spring 2008: Status and Accomplishments.
Real-Time Dissemination of Hurricane Wind Fields Determined from Airborne Doppler Radar John Gamache NOAA/AOML/Hurricane Research Division Collaborators:
The height the end of the pump arm is above the ground is given by the equation H = 6 + 4Sin(πt) Oil Pump Problem where t = time in minutes And H is the.
Noise is estimated [NEXRAD technical manual] at elevation >20  and scaled. Data with low Signal/Noise are determined and censored (black or white on PPI).
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.
Dual-Polarization and Dual-Wavelength Radar Measurements Vivek National Center for Atmospheric Research Boulder, Colorado I.Polarization and dual- wavelength.
Reflectivity and Radial Velocity
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.
Angela Rowe and Robert Houze, Jr. University of Washington 37 th Conference on Radar Meteorology Norman, OK 15 September 2015 Polarimetric radar observations.
S-Band Radar Dual-Polarization Observations of Winter Storms P. C. Kennedy and S. A. Rutledge CSU-CHILL Radar Facility.
National S&T Center for Disaster Reduction Rainfall estimation by BMRC C-Pol radar ICMCS-V Lei FengBen Jong-Dao Jou 1 Lei Feng and 1,2 Ben Jong-Dao.
Surveying 1 / Dr. Najeh Tamim CHAPTER 5 ANGLES, DIRECTIONS, AND ANGLE MEASURING EQUIPMENT.
Curious Precipitation Curtains within the Inflow Region of a Supercell Thunderstorm: A Status Report Rodger A. Brown NOAA/National Severe Storms Laboratory,
METR February Radar Products More Radar Background Precipitation Mode: -Volume Coverage Patterns (VCP) 21: 9 elevation angles with a complete.
Dual-Polarization Radars
Radar Requirements David J. Stensrud NOAA/National Severe Storms Laboratory 2013 Warn-on-Forecast Workshop and Technical Guidance Meetings.
DOPPLER SPECTRA OF WEATHER SIGNALS (Chapter 5; examples from chapter 9)
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.
Atmospheric profile and precipitation properties derived from radar and radiosondes during RICO Louise Nuijens With thanks to: Bjorn Stevens (UCLA) Margreet.
Kavaya-1 Coherent Doppler Lidar Roadmap to Both the NRC Decadal Survey “Science Demonstration” and “Operational” Missions Michael J. Kavaya Jirong Yu Upendra.
90 Vertical Horizontal Oblique line a b Angles a + b = 180 o Angles at a Point b = 115 o Angle a = 180 – 115 = 65 o.
Representing Climate Data II Satellite Imagery and Radar.
The evaluation of updrafts in the Unified Model using single-Doppler radar measurements Nicol JC a, Hogan RJ b, Stein THM b, Hanley KE c, Lean HW c, Plant.
Estimating Rainfall in Arizona - A Brief Overview of the WSR-88D Precipitation Processing Subsystem Jonathan J. Gourley National Severe Storms Laboratory.
Complex Form of Fourier Series For a real periodic function f(t) with period T, fundamental frequency where is the “complex amplitude spectrum”.
NPOL Olympex Located N/ W, 157 m ASL
Development of Assimilation Methods for Polarimetric Radar Data
Representing Climate Data II
the University of Oklahoma
Examples of spectral fields
Thermal Wind, Temperature Advection, and Doppler
Unit 1 – Conic Sections Section 1.4 – The Ellipse Calculator Required
Thermal Wind, Temperature Advection, and Doppler
Radars in Helsinki Testbed
Representing Climate Data II
Presentation transcript:

Zdr for chosen spectral coefficients in , clear-air, day time, south wind, insects, clutter. S.Bachmann

Spectrum one elevation scan az N = IQIQ Radial 1 Radial N Radial az Z dr 128 pulses - - Horizontal  Vertical HVHV

Spectrum one elevation scan az N = IQIQ Radial 1 Radial N Radial az Z dr 128 pulses - - Horizontal  Vertical HVHV Get rid of DC I ' Q' Estimate Spectral Coef SC=f(az, v) header Center of Spectral Coef. GCFGCF Window Spectral observation Window

Spectrum one elevation scan az N = IQIQ Radial 1 Radial N Radial az Z dr 128 pulses - - Horizontal  Vertical HVHV Get rid of DC I ' Q' Estimate Spectral Coef SC=f(az, v) header Center of Spectral Coef. GCFGCF Window v, h) Spectral observation Sounding

Z dr for the original spectrum (all 128 pulses included in calculations) for the chosen spectral window (21 pulses), s.t. the center of spectral window assumes sin- azimuthal dependence for the chosen spectral window (21 pulses), s.t. the center is chosen in agreement with azimuthal and height dependence from sounding.

0.5° 1.5° 2.5° all 128 pulseswindow 21 pulses original GSf GSf, DCf, f(h) GSf, DCf

sounding gives High Zdr vanish at second layer (circled) - birds 128, GSf window, GSf, DCf, f(h) window, GSf, DCf

4.5° 2.5° 1.5° 0.5° GCf, DCf Window(40-55) 180°

Zdr window < Zdr 128 more Birds/insects/both? If Zdr birds (-1..4), insects (0..10)

from Ryzhkov: Biological scatterers in atmosphere InsectsBirds Z (dBZ) 5 – 205 – 30 Z DR (dB) 0 – 12-2 – 3 ρ hv 0.5 – 0.8 δ (°)0 – 1200 – 40 K DP (°/km) Low & noisy ρ hv 0 δ