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Spatial correlation of foF2 and vTEC under quiet and disturbed ionospheric conditions: A case study

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Języki publikacji
EN
Abstrakty
EN
The spatial variations of the ionospheric F2-layer vertical incidence critical frequency (foF2) and GPS-derived vertical total electron content (vTEC) under geomagnetically quiet and disturbed days are examined using measurements from the latitudinal and longitudinal chains of ionospheric stations and GPS receivers over the European area. Plots produced for January 2005 are used to discuss temporal structures in terms of the prevailing solar-terrestrial conditions. Then the line trends procedure has been applied to simultaneous data collected from a limited number of measuring stations during quiet monthly median ionospheric conditions as well as during the storm period of 16-23 January 2005. The procedure is explained involving an application of the least squares method to define latitudinal and longitudinal dependence of foF2 and vTEC at different locations. Examples of coefficients of determination thereby produced show that the linear regression equations are very helpful in predicting longitudinal and latitudinal vTEC and foF2 variations during the quiet as well as disturbed ionospheric conditions.
Czasopismo
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Strony
410--423
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Bibliografia
  • Bradley, P.A., 1995, COST 238 PRIME (Prediction and Retrospective Ionospheric Modelling over Europe) Final Report, Commission of the European Communities, ECSC-EECEAEC, Brussels.
  • Cander, L.R., 1993, On the global and regional behavior of the mid-latitude ionosphere, J. Atmos. Terr. Phys. 55, 11/12, 1543- 551.
  • Cander, L.R., and L. Ciraolo, 2002, First step towards specification of plasmasphericionospheric conditions over Europe on-line, Acta Geod. Geoph. Hung. 37, 153-161.
  • Ciraolo, L., 1993, Evaluation of GPS L2-L1 biases and related daily TEC profiles, Proc. GPS/Ionosphere Workshop, Neustrelitz, 90-97.
  • Ciraolo, L., 2000, Results and problems in GPS TEC evaluation, Proc. Radio Communications Research Units 1st GPS TEC Workshop, Chilton, 47-60.
  • Dow, J.M., R.E. Neilan and G. Gendt, 2005, The International GPS Service (IGS): Celebrating the 10th Anniversary and Looking to the Next Decade, Adv. Space Res. 36, 3, 320-326, doi:10.1016/j.asr.2005.05.125.
  • Kersley, L., D. Malan, E.S. Pryse, L.R. Cander, R.A. Bamford, A. Belehaki, R. Leitinger, S.M. Radicella, C.N. Mitchel and P.S.J. Spencer, 2004, Total electron content - A key parameter in propagation: measurement and use in ionospheric imaging, Ann. Geophys. 47, 1067-1091.
  • Mendillo, M., and J.A. Klobuchar, 2006, Total electron content: Synthesis of past storm studies and needed future work, Radio Sci. 41, RS5S02, doi: 10.1029/2005RS003394.
  • Piggott, W.R., and K. Rawer, 1972, URSI handbook of ionogram interpretation and reduction, World Data Center A for Solar-Terrestrial Physics, Report UAG-23, Environmental Data Service, Asheville, North Carolina, US Department of Commerce, NOAA.
  • Prölss, G.W., 1995, Ionospheric F region storms. In: H. Volland (ed.), "Handbook of Atmospheric Electrodynamics", CRC Press, Boca Raton, FL, 195-248.
  • Samardjiev, T., P.A. Bradley, L.R. Cander and M.I. Dick, 1993, Ionospheric mapping by computer contouring techniques, Electronics Lett. 29, 20, 1794-1795.
  • Stanisławska, I., G. Juchnikowski, L.R. Cander, L. Ciraolo, P.A. Bradley and Z.A. Zbyszyński, 2002, The kriging method of TEC instantaneous mapping, Adv. Space Res. 29, 6, 945-948.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0021-0033
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