Geostationary-satellite beacon-receiver array for studies of ionospheric irregularities
Ionospheric irregularities can be studied by various techniques. These include widely spaced Doppler sounders or ionosondes, Faraday rotation polarimetry, and two-frequency differential Doppler, and radio interferometry. With geostationary satellites, one usually uses Faraday rotation of the beacon signal to measure the ionospheric TEC. With a network of polarimeters, the horizontal wave parameters of Traveling Ionospheric Disturbances (TIDS) can be deduced, but the shortcoming of this technique is its poor sensitivity. This paper describes a geostationary-satellite beacon-receiver array at Los Alamos, New Mexico, which will be employed for the studying of ionospheric irregularities, especially the fine-scale TIDS.
- Research Organization:
- Los Alamos National Lab., NM (United States)
- Sponsoring Organization:
- USDOE; USDOE, Washington, DC (United States)
- DOE Contract Number:
- W-7405-ENG-36
- OSTI ID:
- 7184600
- Report Number(s):
- LA-UR-92-2125; CONF-9207118-1; ON: DE92018979
- Resource Relation:
- Conference: Beacon satellite symposium, Boston, MA (United States), 5-12 Jul 1992
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
GENERAL PHYSICS
TRAVELLING IONOSPHERIC DISTURBANCE
INTERFEROMETRY
DATA ACQUISITION SYSTEMS
DATA PROCESSING
DETECTION
LOS ALAMOS
RADAR
SATELLITES
SIGNAL CONDITIONING
SIGNALS
DEVELOPED COUNTRIES
DISTURBANCES
FEDERAL REGION VI
IONOSPHERIC STORMS
MEASURING INSTRUMENTS
NEW MEXICO
NORTH AMERICA
PROCESSING
RANGE FINDERS
URBAN AREAS
USA
661320* - Auroral
Ionospheric
& Magnetospheric Phenomena- (1992-)