Work Package 2 – Overview of instrumentation, data gathering and calibration issues Calibration of the Galileo 94GHz radar – two years of data Nicolas.

Slides:



Advertisements
Similar presentations
The Important Thing About By. The Important Thing About ******** The important thing about ***** is *****. It is true s/he can *****, *****, and *****.
Advertisements

Robin Hogan, Chris Westbrook University of Reading Lin Tian NASA Goddard Space Flight Center Phil Brown Met Office Why it is important that ice particles.
Ewan OConnor, Robin Hogan, Anthony Illingworth, Nicolas Gaussiat Liquid water path from microwave radiometers.
Ewan OConnor, Robin Hogan, Anthony Illingworth, Nicolas Gaussiat Radar/lidar observations of boundary layer clouds.
Radar/lidar observations of boundary layer clouds
Blind tests of radar/lidar retrievals: Assessment of errors in terms of radiative flux profiles Malcolm Brooks Robin Hogan and Anthony Illingworth David.
The Chilbolton Observatory: Contribution to Key Science Issues Robin Hogan and Anthony Illingworth (Thanks to staff at RAL-STFC and the Met Office)
RA-2 & MWR QWG meeting – ESA/ESRIN – 24 March, 2003 Envisat RA-2 and MWR Events since October 2002 Pierre Féménias ESA/ESRIN.
Exploiting multiple scattering in CALIPSO measurements to retrieve liquid cloud properties Nicola Pounder, Robin Hogan, Lee Hawkness-Smith, Andrew Barrett.
Review of model/obs/products. Models Fluxes –ECMWF fluxes will added v soon (Openshaw) UKMO Global model data –In testing –Damian to provide more data.
Nicolas Gaussiat and Robin Hogan Progress meeting 4 – Toulouse – Oct 2003 Dual wavelength retrieval of LWC and IWC at Chilbolton.
LIGO-G Z Update on the Analysis of S2 Burst Hardware Injections L. Cadonati (MIT), A. Weinstein (CIT) for the Burst group Hannover LSC meeting,
Foreground cleaning in CMB experiments Carlo Baccigalupi, SISSA, Trieste.
Calamari’s Design Decisions Kamin Whitehouse June 18, 2003.
Robin Hogan Anthony Illingworth Marion Mittermaier Ice water content from radar reflectivity factor and temperature.
Work Package 2 – Overview of instrumentation, data gathering and calibration issues Lidar Calibration Ewan O’Connor, Anthony Illingworth and Robin Hogan.
McDaniels – Oct 24, Outline MRI Image uncertainty Point uncertainty ADC uncertainty.
Stochastic Resonance n Adding Noise to a signal can help in its detection. n Just the right amount of noise must be added (resonance) n SR in Nature –Periodic.
Radar: Acronym for Radio Detection and Ranging
Signal vs Noise: Image Calibration First… some terminology:  Light Frame: The individual pictures you take of your target.  Dark Frame: An image taken.
Spectrum Analyzer Basics Copyright 2000 Agenda Overview: What is spectrum analysis? What measurements do we make? Theory of Operation: Spectrum analyzer.
Spectrum Analyzer Basics Copyright 2000 Agenda Overview: What is spectrum analysis? What measurements do we make? Theory of Operation: Spectrum analyzer.
Why We Care or Why We Go to Sea.
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.
Spaceborne Radar for Snowfall Measurements
Calor 2002, march 2002Auguste Besson1 Argon purity measurement of the D0 calorimeter Auguste Besson (ISN - Grenoble) for the D0 collaboration 10.
Gigabit Ethernet EE 164 Group 2 – Presentation 7 Ungtae Lee April 8th 2004.
Accuracy: The closeness of a measurement to the true or actual value
Gerd-Jan van Zadelhoff & Dave Donovan Comparing ice-cloud microphysical properties using Cloudnet & ARM data.
New Results on the Midnight Temperature Maximum for mid-latitudes R. Mesquita (1), J. Meriwether (1), S. Sanders (1), J. Makela (2), D. Fisher (2). SITELatitude.
Survey Toolbox & Plume Detection Toolbox
Chapter 3 Math Toolkit. 3.1~3.2 Significant Figures & in Arithmetic.
Cabauw Experimental Site for Atmospheric Research - CESAR - Henk Klein Baltink Atmospheric Research Section.
WFPC2 UPDATE TIPS : August 15, 2002 L.M. Lubin New WFPC2 Documentation 1.Cycle 12 Instrument Handbook (V7.0, Biretta et al.)  Updated information on the.
The Very Small Array Angela Taylor & Anze Slosar Cavendish Astrophysics University of Cambridge.
Scattering and attenuation and tracking uncertainties for cal/val.
KNMI 35 GHz Cloud Radar & Cloud Classification* Henk Klein Baltink * Robin Hogan (Univ. of Reading, UK)
PR-2 Radar in Aguadilla Ricardo Ríos Olmo Advisor: Dr. José Colom.
Initial Evaluation of the HIAPER Cloud Radar Doppler Velocity Measurements S. M. Ellis, J. Vivekanandan, P. Tsai, E. Loew, C. Burghart, M. Dixon, J. Emmett,
Tests of STO IF Components S. Weinreb April 15, 2009 Two 1-2 GHz IF amplifier plates and one 5 GHz converter plate for the Texas test flight have been.
Experimental Methods for Determining Photodetector Working Points By: Victor Rykalin Mike Smith Jim Maloney.
Recent Advances in Applied Seismology: Exploration Presenter AL-SALEM, M Seminar Consultant and Coordinator Dr.Ali Osman Oncel Case Work 1 Methods for.
Robin Hogan Anthony Illingworth Marion Mittermaier Ice water content from radar reflectivity factor and temperature.
Calibration of PPTA Data R. N. Manchester Australia Telescope National Facility, CSIRO Sydney Australia Summary Effect of calibration on timing Non-linearities.
Nicolas Gaussiat, Anthony Illingworth and Robin Hogan Beeskow, 12 Oct 2005 Liquid Water Path from radiometers and lidar.
Angela Rowe Radar Breakout Session DYNAMO Workshop, Kona, Hawaii 5 March 2013.
Page The Effect of AWGN on the Accuracy of Time of Arrival Detection Rick Enns IEEE a July 2004.
Temporal Classification and Change Detection
Why the construction of isotropic antenna is impracticable.
Siwon Jang Hoyeong Jeong Glenn Christian Talitha Bromwich
Copyright © American Speech-Language-Hearing Association
AC-9/AC-S data analysis from CDOM Lab
Final exam information
May GHz Sharing Study David Baddeley, Motorola SPS.
Chemistry 381 Advanced Module in Physical Chemistry Objectives:
HERA Imaging and Closure
High-denisty DOT system.
Stochastic Resonance Adding Noise to a signal can help in its detection. Just the right amount of noise must be added (resonance) SR in Nature Periodic.
ARM Validation Data for Climate Models
Solving Inequalities Using Addition and Subtraction
Henk Klein Baltink Atmospheric Research Section
Spaceborne Radar for Snowfall Measurements
TARA data for CloudNet H. Russchenberg , O. Krasnov Delft University of Technology – IRCTR, The Netherlands.
Satish Pradhan Dnyanasadhana College, Thane. Department of Chemistry S
Just when you thought you were
Adding and subtracting fractions
Cloud liquid water and ice content by multi-wavelength radar
Open Research and Future Standard Opportunities
Radiometer retrievals of LWP
Presentation transcript:

Work Package 2 – Overview of instrumentation, data gathering and calibration issues Calibration of the Galileo 94GHz radar – two years of data Nicolas Gaussiat and Robin Hogan Progress meeting 3 –Reading – Oct 2002

Calibration technique (Robin et al. paper) Radome attenuation Calibrated Uncalibrated 8 dBZ Zcal

Calibration results Calibration constant to be added to the raw data (+/- 1dB) 3 data acquisition systems working together Robin’s calibration by comparing with 3 GHz radar nicely confirmed From May 1999 to March 2002

Coherent processing : toward more accuracy ? 1 sec average 30 sec average

Identified problem : Noise subtraction vs. peak detection Measured signal power ~ True signal power Measured signal power << True signal power

Data availability Covering period : March 2001 – March 2002 Monthly.tar.gz files : Coherent processing: YYYYMM_chilbolton-galileo.tar.gz Incoherent processing: YYYYMM_chilbolton-galileo_i.tar.gz