1 AIR FORCE RESEARCH LABORATORY Dr. Keith Groves Space Weather Center of Excellence AFRL/VSBXI 29 Randolph Rd Hanscom AFB, MA +1-617-549-7067 voice +1-781-377-3550.

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Presentation transcript:

1 AIR FORCE RESEARCH LABORATORY Dr. Keith Groves Space Weather Center of Excellence AFRL/VSBXI 29 Randolph Rd Hanscom AFB, MA voice fax GPS Support to the MWA Low Frequency Demonstrator

2 AFRL-Supplied GPS Receivers Uses selected low-noise ovenized oscillator for superior low-jitter phase measurements Record raw 50 Hz I/Q data (L1 only) or lower cadence (1-sec, 10-sec, 30- sec) processed parameters (TEC, carrier phase, code, etc.) Not set-up for differential use, but will accept external oscillator Unit provides essentially no visible feedback that it is operating properly Mated with 20-m LMR-400 cable (3.5 dB loss; up to 10 dB acceptable) Three Novatel (GSV) 4004B Ionospheric Scintillation and TEC Monitors

3 Current Real-Time GPS Display

4 Present and anticipated thru 2008* SCINDA Ground Stations 30N 0 30S 210E 240E 270E 300E330E 0 30E 60E90E120E 150E Existing SitesUN IHY SitesOther/collaboration *Future sites shown represent approximate desired locations; actual sites TBD Novatel 4004B

5 TEC from Ascension & Kwajalein Halloween 2006 Receiver bias calibration performed using data from LT when gradients are minimum Technique optimal for mid-latitude sites, but absolute values will still be no better than ~1+ TEC unit 2.7 usec (267 ) delay at 100 MHz

Group Delay as a function of TEC  100% day-to-day variation at equatorial latitudes  Delay increase by X3 for low elevation angles (long slant paths) Daily Variation of TEC

7 Novatel Pinwheel antenna maintains good sensitivity at low elevation angles –Vulnerable to multi- path effects in “non- pristine” environment MWA site topography ideal for GPS –Care should be taken in installation (ground- plane, etc.)

8 Ionospheric Dielectric Properties Nominal dielectric permittivity in “smooth” ionosphere Linearized description when weak density fluctuations are present Permittivity has a direct dependence on total  N “Roughness” of mid-latitude ionosphere has never been carefully studied (standard techniques insensitive to irregularities except during storm-induced activity) MWA has sensitivity to perform routine measurements

9 Summary GPS sensors will provide good estimates of ionospheric TEC at MWA –May want to consider operating receivers with common external oscillator signal to guarantee “coherent” GPS measurements across aperture Unprecedented mid-latitude ionospheric structure studies possible with MWA –Relevant for proposed space-based UHF/VHF coherent synthetic aperture radar (SAR) systems