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Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 222995 bytes)
GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 5,
1255,
doi:10.1029/2002GL015496,
2003
Incoherent scatter radar plasma density measurements at Jicamarca using a transverse-mode differential-phase method
Erhan Kudeki
Department of Electrical and Computer Engineering,
University of Illinois at Urbana-Champaign,
Urbana,
Illinois,
USA
Ronald F. Woodman
Instituto Geofisico del Peru,
Lima,
Peru
Zhaomei Feng
Department of Electrical and Computer Engineering,
University of Illinois at Urbana-Champaign,
Urbana,
Illinois,
USA
Abstract
The 50 MHz Jicamarca incoherent scatter radar can be used to make very high precision F-region plasma drift measurements with
less than a m/s uncertainty and 5 min/15 km time/height resolutions. In such measurements the transmitting antenna beam is
pointed perpendicular to the geomagnetic field [e.g.,
Kudeki et al., 1999
] and backscattered fields consist of magneto-ionic O- and X-components with unequal phase retardations. Detecting the fields
with an orthogonal pair of linear-polarized antennas and fitting the average power and differential-phase of the antenna outputs
to an appropriate data model we have succeeded in making F-region electron density measurements with data collected during
Jicamarca drifts experiments. This procedure provides Jicamarca with a new capability for simultaneous drifts and density
measurements at F-region heights.
Published 14
March
2003.
Index Terms: 6969 Radio Science: Remote sensing; 2415 Ionosphere: Equatorial ionosphere; 6934 Radio Science: Ionospheric propagation (2487); 6994 Radio Science: Instruments and techniques.
Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 222995 bytes)
Citation: Kudeki, E., R. F. Woodman, and Z. Feng
(2003),
Incoherent scatter radar plasma density measurements at Jicamarca using a transverse-mode differential-phase method,
Geophys. Res. Lett.,
30(5),
1255,
doi:10.1029/2002GL015496.
Copyright 2003 by the American Geophysical Union.
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