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RADIO SCIENCE,
VOL. 35, NO. 3,
PAGES 885–904,
2000
The application of GPS observations to equatorial aeronomy
Michael Mendillo
Center for Space Physics, Boston University, Boston, Massachusetts
Bosheng Lin
Center for Space Physics, Boston University, Boston, Massachusetts
Jules Aarons
Center for Space Physics, Boston University, Boston, Massachusetts
Abstract
Routine observations of the ionospherically imposed propagation effects upon GPS satellite signals are available online from
the International GPS Service for Geodynamics. With over 200 ground-based stations now reporting data, ionospheric studies
ranging from the analysis of single-site observations to the full global network have demonstrated the geophysical science
yield possible from this remarkable resource. In this paper we expand on the use of GPS data for comprehensive “regional studies”
at low latitudes. Using the GPS observing sites in South America, we show how routine observations are processed to form reliable
total electron content (TEC) values capable of describing the latitudinal, longitudinal, local time, and storm time behavior
over the full span of the continent. To study the dominant F region structure at low latitudes, the Appleton anomaly, two indices are developed to assess its strength (Is ) and asymmetry (Ia ). TEC data at 30 s intervals are used to form phase fluctuation indices that capture plasma irregularity patterns at 15-min
(f p ) and hourly (F p ) time resolution. Tests of F p at Atlantic and Pacific sector locations show them to reproduce accurately all known occurrence patterns for equatorial spread
F (ESF). The use of the three indices (I s ,I a , and F p ) to formulate predictive capabilities for ESF on the basis of the enhancement or suppression of growth rate indicators was
not particularly successful.
Received 18
May
1999;
accepted 3
January
2000.
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Citation: Mendillo, M., B. Lin, and J. Aarons
(2000),
The application of GPS observations to equatorial aeronomy,
Radio Sci.,
35(3),
885–904.
Copyright 2000 by the American Geophysical Union.
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