slide 1 German Aerospace CenterMicrowaves and Radar Institute Extraction of clear-air wind Dr. Thomas Börner DLR Oberpfaffenhofen.

Slides:



Advertisements
Similar presentations
Institut für Physik der Atmosphäre POLDIRAD and LINET observations during COPS Martin Hagen and Hartmut Höller DLR Oberpfaffenhofen.
Advertisements

1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005.
Presented By: Usama Ashraf ID: Terminal Doppler Weather Radar (TDWR): TDWR is a doppler weather radar system used primarily for the detection.
7. Radar Meteorology References Battan (1973) Atlas (1989)
ATS 351 Lecture 9 Radar. Radio Waves Electromagnetic Waves Consist of an electric field and a magnetic field Polarization: describes the orientation.
Echo Tops Fairly accurate at depicting height of storm tops Inaccurate data close to radar because there is no beam angle high enough to see tops. Often.
OBSERVATIONAL VALIDATION OF AVIAN RADAR SYSTEMS Wendell Bunch Edwin Herricks, PhD.
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.
Contributors to Measurement Errors (Chap. 7) *1) Widespread spatial distribution of scatterers (range ambiguities) *2) Large velocity distribution (velocity.
Review of the current and likely future global NWP requirements for Weather Radar data Enrico Fucile (ECMWF) Eric WATTRELOT & Jean-François MAHFOUF (Météo-France/CNRM/GMAP)
Operational Weather Radar Featuring: WSR-88D Doppler Radar
Folie 1 Ambiguity Suppression by Azimuth Phase Coding in Multichannel SAR Systems DLR - Institut für Hochfrequenztechnik und Radarsysteme F. Bordoni, M.
Advanced Radio and Radar
Folie 1 Performance Investigation on the High-Resolution Wide-Swath SAR System Operating in Stripmap Quad-Pol and Ultra-Wide ScanSAR Mode DLR - Institut.
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Remote Sensing Technology Institute Extraction of the surface velocity of rivers with SAR- ATI H. Runge 1, S. Suchandt 1, R. Horn 2, T. Eiglsperger 3 German.
QUANTITATIVE APPLICATIONS OF BROADCAST MEDIA WEATHER RADAR DATA Neil I. Fox Department of Atmospheric Science University of Missouri-Columbia Columbia,
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)
COPS-GOP-WS3 Hohenheim 2006_04_10 Micro- Rain- Radar Local Area Weather Radar Cloud Radar Meteorological Institute University Hamburg Gerhard Peters.
Feature Subset Selection using Minimum Cost Spanning Trees Mike Farah Supervisor: Dr. Sid Ray.
Institut für Physik der Atmosphäre POLDIRAD Polarization Diversity Doppler Radar Martin Hagen DLR Oberpfaffenhofen.
Topic 4 Radar Fundamentals Enabling Objectives 4.1 DISCUSS the classifications of radars and specific radar systems employed by military and civilian users.
slide 1 German Aerospace CenterMicrowaves and Radar Institute Methodology for obtaining physical parameters from fully polarimetric.
Analysis of Three Dimensional Wind Fields from Two Operational Radars Yong Kheng Goh* and Anthony Holt * Doppler radar and wind-field.
Radar: Acronym for Radio Detection and Ranging
Surveillance Weather Radar 2000 AD. Weather Radar Technology- Merits in Chronological Order WSR-57 WSR-88D WSR-07PD.
Doppler Radar From Josh Wurman Radar Meteorology M. D. Eastin.
Spaceborne Weather Radar
Spaceborne Radar for Snowfall Measurements
RADAR Detection of Extensive Air Showers Nils Scharf III. Physikalisches Institut A Bad Honnef Nils Scharf III. Physikalisches Institut A Bad.
RADAR METEOROLOGY Yrd. Doç. Dr. Ali DENİZ. OUTLINE INTRODUCTION RADAR HARDWARE ELECTROMAGNETİC WAVES RADAR EQUATION FOR POINT TARGETS METEOROLOGICAL TARGETS.
A Doppler Radar Emulator and its Application to the Detection of Tornadic Signatures Ryan M. May.
Phased Array Radar Configurations for Ground-Based and Airborne Deployments Dual Use: Deployable on airborne and ground-based platforms Key measurements:
International Research Centre for Telecommunications and Radar High resolution 3D wind profiling using an S-band polarimetric FM-CW radar: dealiasing techniques.
GISMO Simulation Study Objective Key instrument and geometry parameters Surface and base DEMs Ice mass reflection and refraction modeling Algorithms used.
CARPE-DIEM 13/6/02, slide 1German Aerospace Center Microwaves and Radar Institute CARPE-DIEM Besprechung Helsinki, June 2004 Ewan.
Study Design and Summary Atmospheric boundary layer (ABL) observations were conducted in Sapporo, Japan from April 2005 to July Three-dimensional.
TAMDAR Winds Some results from a study of the ATReC/AIRS-II Campaign Data Robert Neece, NASA Langley Research Center.
Basic Principles of Doppler Radar Elena Saltikoff Alessandro Chiariello Finnish Meteorological Institute.
Introduction Acknowledgements Funding for the CSU-MAPS is provided through a joint NSF-MRI R 2 grant (AGS# , ) awarded to San Francisco and.
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).
The new DWD polarimetric weather radar network: a new radar data processing framework and new products Michael Frech 1, Nils Rathmann 2, Jörg Steinert.
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.
Institute of Atmospheric Physics Fast Calibration of Weather Radar Systems for Multi Polarization Radar Measurements Jens Reimann, Martin Hagen DLR-Institute.
Where are the radars located? What is the radar coverage?
Reflectivity and Radial Velocity
EumetCal Examples.
III) CHARACTERISTICS OF THE ADDED CLUTTER RAIN MeteoSvizzera, 6605 Locarno, Switzerland Simulation.
Microwaves and Radar Aerospace Center Polarimetric Bistatic X-Band Measurement Facility and its Applications Dr. Thomas.
Quality Control Problems For VAD Winds and NEXRAD Level-II Winds In the Presence of Migrating Birds Li Bi 1, Alan Shapiro 1,2, Pengfei Zhang 3 and Qin.
RADAR METEOROLOGY Courtney Schumacher Texas A&M University ATMO 352.
LiDAR ApplicationsOverview
Range & Doppler Accuracy by Ramya R.
EEE381B Pulsed radar A pulsed radar is characterized by a high power transmitter that generates an endless sequence of pulses. The rate at which the pulses.
Radar Interpretation Chad Entremont National Weather Service Jackson, MS.
PRESENTATION OUTLINE Experiment Objective Introduction Data Conclusion Recommendations.
Radar Range Equation.
What is Doppler Weather Radar
RENISH THOMAS (GPM) Global-Precipitation- Mapper
Weather Radar.
An overview by: Thomas Jones December 2, 2002
Transmission Frequency
the University of Oklahoma
Developed by Eastwood Im Jet Propulsion Laboratory
Advanced Radar Systems
Final Project: Phase Coding to Mitigate Range/Velocity Ambiguities
S-Pol Radar Deployment
Spaceborne Radar for Snowfall Measurements
1st Annual Israel Multinational BMD Conference & Exhibition
Presentation transcript:

slide 1 German Aerospace CenterMicrowaves and Radar Institute Extraction of clear-air wind Dr. Thomas Börner DLR Oberpfaffenhofen Microwaves and Radar Institute D Weßling

slide 2 German Aerospace CenterMicrowaves and Radar Institute Outline Introduction to clear air data Purpose of this study Possible parameters for DLR's POLDIRAD Analysis of the data set, results Conclusions

slide 3 German Aerospace CenterMicrowaves and Radar Institute Introduction to clear air data In Europe, weather radar is primarily used to measure precipitation over large areas. Wind measurements are a secondary benefit, not seen as the primary role.  Quality of wind data is usually less than optimal! Reason: low power and lack of sensitivity Clear air echoes detectable at max. ranges: km. Exact cause is still subject to speculation. Evidence suggests: insects and birds! High Z DR values: 5-10 dB. Best performance during summer until autumn.

slide 4 German Aerospace CenterMicrowaves and Radar Institute Purpose of this study Original intention: search for new possibilities of processing the data to increase the quality of clear air wind measurements. Problem: during summer there was still no unprocessed (raw) data available, only final products. Workaround: collect data with as many different sensor setup parameters (PRF, resolution, etc.) as possible.  Find the best combination for clear air measurements!

slide 5 German Aerospace CenterMicrowaves and Radar Institute Possible parameters for DLR's POLDIRAD PRF: 400 Hz, 800 Hz, 1200 Hz Pulse length: 1 µs, 2 µs (only for PRF = 400 Hz) Resolution (bin length): 150 m, 300 m Number of samples per bin: 32, 64, 128 Elevation: any angle, chosen 1° and 2°  Total of 48 possible combinations!

slide 6 German Aerospace CenterMicrowaves and Radar Institute Z – PRF behavior (300 m, 1 µs, 128 samp.) 400 Hz 800 Hz 1200 Hz

slide 7 German Aerospace CenterMicrowaves and Radar Institute V – PRF behavior (300 m, 1 µs, 128 samp.) 400 Hz 800 Hz 1200 Hz

slide 8 German Aerospace CenterMicrowaves and Radar Institute Z – samp. behavior (300 m, 1 µs, 1200 Hz) 32 samples 64 samples 128 samples

slide 9 German Aerospace CenterMicrowaves and Radar Institute V – samp. behavior (300 m, 1 µs, 1200 Hz) 32 samples 64 samples 128 samples

slide 10 German Aerospace CenterMicrowaves and Radar Institute V – res. behavior (1200 Hz, 1 µs, 128 samp.) 150 m300 m

slide 11 German Aerospace CenterMicrowaves and Radar Institute V – elev. behavior (1200 Hz, 1 µs, 128 samp.) 1°2°

slide 12 German Aerospace CenterMicrowaves and Radar Institute Scanning Time The total time to scan one full PPI increases for –lower PRF –higher number of samples –higher resolution –higher pulse length  important if the weather situation changes rapidly (or if there are strong local turbulences) and has to be scanned in short intervals.

slide 13 German Aerospace CenterMicrowaves and Radar Institute “Quality” or Accuracy Insects and birds can develop considerable speeds relative to the wind, which add to the measured radial wind velocities!  Insects:up to 6 m/s.  Birds:up to 15 m/s. Clear air wind velocities have therefore to be handled with care. However, polarimetric signatures of these objects can help in the areas of entomology and ornithology in order to track and also classify aerial plankton.

slide 14 German Aerospace CenterMicrowaves and Radar Institute Conclusions Best combination of parameters: –PRF: 1200 Hz –number of samples: 128 –resolution: 150 m –pulse length: N/A –elevation: as close to the ground as possible If time is of concern, the recommendation is to reduce the resolution and/or the number of samples.