Detection of high-altitude ionospheric irregularities with GPS/MET

Details Detection of high-altitude ionospheric irregularities with GPS/MET Detection of high-altitude ionospheric irregularities with GPS/MET

Feb 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29c...3s&link_type=abstract

Geophysical Research Letters, Volume 29, Issue 3, pp. 3-1, CiteID 1033, DOI 10.1029/2001GL013398

Physics

11

Ionosphere: Ionospheric Irregularities, Ionosphere: Wave Propagation (6934), Ionosphere: Instruments And Techniques, Ionosphere: Equatorial Ionosphere

Scientific paper

In this study radio occultation data from the GPS/MET experiment are used for detection of high-altitude ionospheric irregularities. This is done by back propagation of the complex electromagnetic field observed in orbit while accounting for the direction of the Earth's magnetic field. The irregularities are detected mainly in the F region. However, for some occultations they are detected above the F2 peak at altitudes up to 1000 km and higher. Results of numerical simulations, a description of the used algorithm, and examples of the processed GPS/MET data are presented.

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