Inversion of backscatter ionograms and TEC data for over-the-horizon radar

Over‐the‐horizon radar (OTHR) uses ionospheric reflection to propagate HF transmissions to long range (∼500–5000 km). The ionosphere acts as a dynamic “mirror” that varies diurnally, seasonally, and with the solar cycle. Geolocation of targets observed by OTHR (Coordinate Registration (CR)) requires...

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Veröffentlicht in:Radio science Jg. 47; H. 4
Hauptverfasser: Fridman, Sergey V., Nickisch, L. J., Hausman, Mark
Format: Journal Article
Sprache:Englisch
Veröffentlicht: Washington Blackwell Publishing Ltd 01.08.2012
Schlagworte:
Algorithms
Atmospheric sciences
Data collection
Geophysics
inverse problem
Ionosphere
Mathematics
Radar
ISSN:0048-6604, 1944-799X
Online-Zugang:Volltext
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Zusammenfassung:Over‐the‐horizon radar (OTHR) uses ionospheric reflection to propagate HF transmissions to long range (∼500–5000 km). The ionosphere acts as a dynamic “mirror” that varies diurnally, seasonally, and with the solar cycle. Geolocation of targets observed by OTHR (Coordinate Registration (CR)) requires accurate real‐time ionospheric modeling and HF propagation calculations to convert radar‐measured target signal delays and beam steers to geographical position. We merged our backscatter ionogram (BI) leading edge inversion algorithm CREDO with our more advanced ionospheric data assimilation capability, GPS Ionospheric Inversion (GPSII). The combined algorithm produces a dynamic model of electron density for a fixed geographical region. The model is consistent with BI leading edge data, vertical sounding data, as well as with absolute and relative total electron content (TEC) data from a number of GPS/LEO receivers. Incorporation of additional ionospheric data beyond conventional OTHR vertical and oblique backscatter soundings is expected to enhance the fidelity of real‐time ionosphere models, resulting in improved OTHR Coordinate Registration metric accuracy. Initial tests of the OTHR CR supported by the new ionospheric inversion algorithm indicate noticeable improvement of CR accuracy in comparison with legacy techniques. Key Points OTHR coordinate registration requires real‐time ionosphere model Ionospheric model supported by backscatter and vertical ionograms is useful Ionospheric model is further improved by incorporating GPS TEC data
Bibliographie:istex:0822B1AD6CF86E898218CBFB5ECAA34037F7E722
ArticleID:2011RS004932
ark:/67375/WNG-J8CWSBXP-3
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ISSN:0048-6604
1944-799X
DOI:10.1029/2011RS004932