Measuring Signal Strength Measure relative cross section of existing GNSS retroreflector arrays Measure transmitted beam pattern in absolute units using.

Slides:



Advertisements
Similar presentations
5.4 Correlation and Best-Fitting Lines
Advertisements

OUTLINE Motivation Modeling Simulation Experiments Conclusions.
SVN-49 Signal Anomaly Presented by Tom Stansell GPSW POC: Lt. Col. James Lake, Ph.D.
Laser Retro-reflector Arrays on the Compass Satellites Chen WanZhen, Yang FuMin, Wang YuanMing, Li Pu Shanghai Observatory, Chinese Academy of Sciences.
Anisotropy in Cosmic Ray Arrival Directions Using IceCube and IceTop Frank McNally ISCRA.
Time-Lapse Monitoring of CO2 Injection with Vertical Seismic Profiles (VSP) at the Frio Project T.M. Daley, L.R. Myer*, G.M. Hoversten and E.L. Majer.
UPRM Lidar lab for atmospheric research 1- Cross validation of solar radiation using remote sensing equipment & GOES Lidar and Ceilometer validation.
7. Radar Meteorology References Battan (1973) Atlas (1989)
Calibration Scenarios for PICASSO-CENA J. A. REAGAN, X. WANG, H. FANG University of Arizona, ECE Dept., Bldg. 104, Tucson, AZ MARY T. OSBORN SAIC,
KHz Single Photon Ranging: A Precise Tool to Retrieve Optical Response of Satellites Toshimichi Otsubo Hitotsubashi University 16th International Workshop.
1 Extreme Ultraviolet Polarimetry Utilizing Laser-Generated High- Order Harmonics N. Brimhall, M. Turner, N. Herrick, D. Allred, R. S. Turley, M. Ware,
2-3 November 2009NASA Sea Level Workshop1 The Terrestrial Reference Frame and its Impact on Sea Level Change Studies GPS VLBI John Ries Center for Space.
Time Transfert by Laser Link T2L2 On Jason 2 OCA –UMR Gemini Grasse – FRANCE E. Samain – Principal.
Distance observations
Advanced Radio and Radar
Remote sensing in meteorology
Titan’s Thermospheric Response to Various Plasma Environments Joseph H. Westlake Doctoral Candidate The University of Texas at San Antonio Southwest Research.
Summary: Scientific Achievement, Applications and Future Requirements Zueheir Altamimi Steve Klosko Richard Gross Aleksander Brzezinski.
Session Summary to General Assembly Targets and Signatures.
Page 1 1 of 20, EGU General Assembly, Apr 21, 2009 Vijay Natraj (Caltech), Hartmut Bösch (University of Leicester), Rob Spurr (RT Solutions), Yuk Yung.
14 October th International Workshop on Laser Ranging 1 LRO Operations at the MLRS Jerry R. Wiant Randall L. Ricklefs Peter J. Shelus Center for.
METO 621 Lesson 27. Albedo 200 – 400 nm Solar Backscatter Ultraviolet (SBUV) The previous slide shows the albedo of the earth viewed from the nadir.
Per R. Bodin Global Posision System GPS. Per R. Bodin Litt historie 1960: nasA & DoD are Interested in developing a satellite based position system with.
GPS Satellites Satellite-based navigation system originally developed for military purposes (NAVSTAR ). NAVSTAR Global Positioning System (GPS) Globally.
Spaceborne Weather Radar
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Toshimichi Otsubo Mihoko Kobayashi Hitotsubashi University 1 Optical Response Simulation for ASTRO-G Laser Reflector Array Hiroo Kunimori National Institute.
ROUGH SENSITIVITY ESTIMATES USING DIRECT SUN BETWEEN 1.5 AND 2 AIRMASSES AIRMASS CHANGE = 0.5 CO 2 RATIO CHANGE=.024 SINCE 1 AIRMASS IS ~ 380 PPM WE GET.
UNNOFIT inversion V. Bommier, J. Rayrole, M. Martínez González, G. Molodij Paris-Meudon Observatory (France) THEMIS Atelier "Inversion et transfert multidimensionnel",
Chapter 9 Electromagnetic Waves. 9.2 ELECTROMAGNETIC WAVES.
1 Interpreting SECCHI White Light Images: FOV Sensitivity & Stereo Viewing Paulett Liewer, JPL; Russ Howard & Dennis Socker, NRL SECCHI Consortium Meeting.
Numerical Investigation of Internal Wave-Vortex Interactions Tyler D. Blackhurst and J.C. Vanderhoff Department of Mechanical Engineering Brigham Young.
Remote Sensing Microwave Remote Sensing. 1. Passive Microwave Sensors ► Microwave emission is related to temperature and emissivity ► Microwave radiometers.
SeaDAS Training ~ NASA Ocean Biology Processing Group 1 Level-2 ocean color data processing basics NASA Ocean Biology Processing Group Goddard Space Flight.
1 PROPAGATION ASPECTS FOR SMART ANTENNAS IN WIRELESS SYSTEMS JACK H. WINTERS AT&T Labs - Research Red Bank, NJ July 17,
Space Geodesy (1/3) Geodesy provides a foundation for all Earth observations Space geodesy is the use of precise measurements between space objects (e.g.,
Xiong Liu, Mike Newchurch Department of Atmospheric Science University of Alabama in Huntsville, Huntsville, Alabama, USA
An In-depth Look at ICESat and GLAS By: Vishana Ramdeen.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
1 What you will learn today 1. New vocabulary 2. How to determine if data points are related 3. How to develop a linear regression equation 4. How to graph.
Guidance and Navigation
Spaceborne 3D Imaging Lidar John J. Degnan Geoscience Technology Office, Code Code 900 Instrument and Mission Initiative Review March 13, 2002.
Definition and assessment of a regional Mediterranean Sea ocean colour algorithm for surface chlorophyll Gianluca Volpe National Oceanography Centre, Southampton.
1 PHY Lecture 5 Interaction of solar radiation and the atmosphere.
Study of neutrino oscillations with ANTARES J. Brunner.
Study of neutrino oscillations with ANTARES J. Brunner.
SATELLITE ORBITS The monitoring capabilities of the sensor are, to a large extent, governed by the parameters of the satellite orbit. Different types of.
Simulation studies of total absorption calorimeter Development of heavy crystals for scintillation and cherenkov readout Dual readout in the 4 th concept.
Theoretical Centre-of-mass Corrections for LAGEOS, ETALON and AJISAI Toshimichi OTSUBO Communications Research Laboratory, Kashima, Japan Graham M APPLEBY.
INFN-LNF SCF_Lab Optical test facility for payloads in Space simulated conditions 15/04/20161G. Delle Monache for the SCF_Lab team.
Signal Propagation Basics
TPE Contributions to Proton EM Properties in TL Region Dian-Yong Chen Institute of High Energy Physics, Beijing
Date of download: 7/11/2016 Copyright © 2016 SPIE. All rights reserved. (a) Red-free scanning ophthalmoscope image of rabbit retina after infrared irradiation.
Cassini Huygens EECS 823 DIVYA CHALLA.
Active Microwave Remote Sensing
Polyimide sheet (5 mils)) AZ-93 Thermal Paint (5 mils))
Signal Processing Session
Lunar observation data set preparation
Two Interpretations of What it Means to Normalize the Low Energy Monte Carlo Events to the Low Energy Data Atms MC Atms MC Data Data Signal Signal Apply.
S. Rowan, M. Fejer, E. Gustafson, R. Route, G. Zeltzer
Fundamental Physics and applications
Field quality to achieve the required lifetime goals (single beam)
Data Preparation for ASTER
Pulsar 3: Significant peaks, well above the noise
Technician Licensing Class
A. The signal strength of received signals
Remote sensing in meteorology
National Institute for Environmental Studies, Tsukuba, Japan
Presentation transcript:

Measuring Signal Strength Measure relative cross section of existing GNSS retroreflector arrays Measure transmitted beam pattern in absolute units using the sensor on the T2L2 satellite Measure cross section of retroreflector arrays in the laboratory before launch

Why measure signal strength? High altitude GNSS satellites require very high cross section. Present arrays give weak signals Uncoated cubes appear to give higher cross section than coated cubes. ETS-8 uses uncoated cubes but can only be observed from Asian stations. COMPASS uses uncoated cubes and gives global visibility Quantitative signal strength measurements would be helpful for designing future GNSS arrays.

Relative signal strength It is not possible to measure absolute signal strength because of various uncertainties. Relative signal strength can be measured relatively accurately The variation of signal strength with range can be accurately computed Uncertainties in atmospheric models cancel if observations are made at the same zenith angle

Method of analysis Correct observations to a standard range such as 20 megameters Do a semi-log plot of signal strength for each satellite and station vs zenith angle There should be a constant difference (ratio) between the plots for different satellites.

Experiment plan Range to COMPASS, GLONASS, GPS, Giove-A, Giove-B using same system set up Range as often as possible for a few minutes per satellite at a variety of zenith angle Make estimates of relative return rates if possible Deposit full-rate and NP data

T2L2 experiment Calculated and measured signal strengths can differ by an order of magnitude The sensor on T2L2 can measure the signal received at the satellite Measuring the signal strength at the satellite can help determine whether the discrepancies between measured and calculated signal strength are on the uplink or the downlink

Beam pattern Scanning the transmitted beam across the T2L2 satellite can be used to map the transmitted beam pattern The central part of the beam pattern may not contain the total energy due to large angle scattering. Measuring the absolute signal received at the satellite can determine the signal lost to atmospheric absorption or large angle scattering.

Variations in transmitted beam Measurements of the beam pattern received at the T2L2 satellite can be used to study the received energy and beam divergence as a function of: –Atmospheric conditions –Zenith angle –Station parameters Beam divergence is limited by seeing conditions. Variations in seeing conditions can change the beam divergence and signal strength. Narrow beams may be most sensitive to seeing conditions.

Positive and negative dihedral angle offsets in uncoated cubes A dihedral angle offset in an uncoated cube produces an asymmetrical diffraction pattern when linear polarization is used. An equal mixture of positive and negative offsets eliminates the polarization asymmetry. A thermal study suggests that an equal mixture of positive and negative offsets is more stable. Specification of 0.0 +/-.5 arcsec gives angles from -.5 to +.5 arcsec. Specification of.75 +/-.5 arcsec gives angles from.25 to 1.25 arcsec.

No dihedral angle offset Plotted with.24 maximum Uncoated, circular polarization Same as above with.12 maximum (All plots below are.12 max) +.75 arcsec dihedral offset CircularLinear -.75 arcsec dihedral offset Linear Average of +.75 and -.75 Linear Coated 1.5 inch No dihedral offset Plotted with.93 max Scale -50 to +50 µrad No offset Linear

Analysis and testing of uncoated cube corners During the APOLLO program analytical calculations and laboratory tests were done. Analytical programs were developed at SAO in 1971 for the LAGEOS mission. LNF in Italy has thermal vacuum laboratory facilities, thermal modeling program, and optical ray tracing program using CodeV. Reinhart Neubert measured an uncoated cube. Optical ray tracing program recently developed by Toshimichi Otsubo.

LNF Space Climactic Facility Simone Dell’Agnello Spare GPS array (flight qualified) Section of LAGEOS cubes LARES cubes and whole array Russian prototype cube corners Proposed LUNAR cube NASA hollow cube Maintain facility for testing future arrays?