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The structure of the mid- and high-latitude ionosphere during the November 2004 storm event obtained from GPS observations

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
GPS data from the International GNSS Service (IGS) network were used to study the development of the severe geomagnetic storm of November 7-12, 2004, in the total electron content (TEC) on a global scale. The TEC maps were produced for analyzing the storm. For producing the maps over European and North American sectors, GPS measurements from more than 100 stations were used. The dense network of GPS stations provided TEC measurements with a high temporal and spatial resolution. To present the temporal and spatial variation of TEC during the storm, differential TEC maps relative to a quiet day (November 6, 2004) were created. The features of geomagnetic storm attributed to the complex development of ionospheric storm depend on latitude, longitude and local time. The positive, as well as negative effects were detected in TEC variations as a consequence of the evolution of the geomagnetic storm. The maximal effect was registered in the subauroral/auroral ionosphere during substorm activity in the evening and night period. The latitudinal profiles obtained from TEC maps for Europe gave rise to the storm-time dynamic of the ionospheric trough, which was detected on November 7 and 9 at latitudes below 50N. In the report, features of the response of TEC to the storm for European and North American sectors are analyzed.
Czasopismo
Rocznik
Strony
490--508
Opis fizyczny
Twórcy
autor
autor
  • Institute of Geodesy, University of Warmia and Mazury in Olsztyn, Poland, kand@uwm.edu.pl
Bibliografia
  • Balan, N., G.J Bailey and R.B. Nair,. 1991, Solar and magnetic activity effects on the latitudinal variations of TEC enhancement, Ann. Geophys. 9, 60-69.
  • Baran, L.W., I.I. Shagimuratov and N.J. Tepenitsina, 1997, The use of GPS for ionospheric studies, Art. Satellites 32, 49-60.
  • Baran, L.W., I.I. Ephishov and I.I. Shagimuratov, 2001, Ionospheric total electron content behaviour during November 1997 storm, Phys. Chem. Earth C 26, 341-346.
  • Blagoveshchensky, D.V., O.M. Pirog, N.M. Polekh and L.V. Chistyakova, 2003, Mid-latitude effects of the May 15, 1997 magnetic storm, J. Atmos. Sol.-Terr. Phys. 65, 203-210.
  • Buonsanto, M.J., 1999, Ionospheric storms - A review, Space Sci. Rev. 88, 563.
  • Cander, L.R., 1993, On the global and regional behaviour of the mid-latitude ionosphere, J. Atmos. Sol.-Terr. Phys. 55, 1543-1551.
  • Cander, L.R., and S.J. Mihajlovic, 2005, Ionospheric spatial and temporal variations during the 29-31 October 2003 storm, J. Atmos. Sol.-Terr. Phys. 67, 12, 1118-1128.
  • Danilov, A.D., 2001, F2-region response to geomagnetic disturbances, J. Atmos. Sol.-Terr. Phys. 63, 441-449.
  • Danilov, A.D., and J. Lastovicka, 2001, Effects of geomagnetic storms on the ionosphere and atmosphere, Int. J. Geomagn. Aeron. 2, 3, 209-224.
  • Forster, M., A.A. Namgaladze and R.Y. Yurik, 1999, Thermospheric composition changes deduced from geomagnetic storm modeling, Geophys. Res. Lett. 26, 16, 2625-2628.
  • Foster, J.C., 1993, Storm time plasma transport at middle and high latitudes, J. Geophys. Res. 98, A2, 1675-1690, doi:10.1029/92JA02032.
  • Foster, J.C., P.J. Erickson, A.J. Coster, J. Goldstein and F.J. Rich, 2002, Ionospheric signatures of plasmaspheric tails, Geophys. Res. Lett. 29, 13, doi:10.1029/2002GL015067.
  • Fuller-Rowell, T.J., M.V. Codrescu, R.J. Moffett and S. Quegan, 1994, Response of the thermosphere and ionosphere to geomagnetic storms, J. Geophys. Res. 99, A3, 3893-3914.
  • Fuller-Rowell, T.J., M.V. Codrescu, H. Rishbeth, R.J. Moffett and S. Quegan, 1996, On the seasonal response of the thermosphere and ionosphere to geomagnetic storms, J. Geophys. Res. 101, A3, 2343-2353.
  • Fuller-Rowell, T.J., M.V. Codrescu, R.G. Roble and A.D. Richmond, 1997, How does the thermosphere and ionosphere react to a geomagnetic storm? In: B.T. Tsurutani et al. (eds.), "Magnetic Storm", Geophys. Monogr. Series 98, AGU, Washington, D.C., 203-225.
  • Fuller-Rowell, T.J., M.V. Codrescu, E. Araujo-Pradere and I. Kitiev, 1998, Progress in developing a storm-time ionospheric correction model, Adv. Space Res. 22, 6, 821-827.
  • Hernandez-Pajares, M., J.M. Juan and J. Sanz, 1997, High resolution TEC monitoring method using permanent ground GPS receivers, Geophys. Res. Lett. 24, 13, 1643-1646.
  • Ho, C.M., A.J. Manucci, X. Pi, B.T. Tsurutani, L. Sparks, B.A. Iijima, B.D. Wilson, I. Harris and M.J. Reyes, 1998, Global ionosphere TEC variations January 10, 1997 storm, Geophys. Res. Lett. 25, 14, 2589-2592.
  • Horvath, I., and E.A. Essex, 2003, The southern-hemisphere mid- time and night time trough at low-sunspot numbers, J. Atmos. Sol.-Terr. Phys. 65, 917-940.
  • Jakowski, N., E. Putz and P. Spalla, 1990, Ionospheric storm characteristics deduced from satellite radio beacon observations at three European stations, Ann. Geophys. 8, 343-351.
  • Jakowski, N., S. Schlutter and E. Sardon, 1999, Total electron content of the ionosphere during geomagnetic storm on 10 January 1997, J. Atmos. Sol.-Terr. Phys. 61, 299-307.
  • Jakowski, N., V. Wilken, S. Schlueter, S.M. Stankov and S. Heine, 2005, Ionospheric space weather effects monitored by simultaneous ground and space based GNSS signals, J. Atmos. Sol.-Terr. Phys. 67, 12, 1074-1084.
  • Krankowski A., L.W. Baran and I.I. Shagimuratov, 2002, Influence of the northern ionosphere on positioning precision, Phys. Chem. Earth 27, 391-395.
  • Krankowski, A., I.I. Shagimuratov, L.W. Baran and G.A. Yakimova, 2004, Storm-time changes of ionospheric TEC during the November 5, 2001 disturbances, Bulg. Geophys. J. 30, 1-4, 10-22.
  • Lastovicka, J., 2002, Monitoring and forecasting of ionospheric space weather-effects of geomagnetic storms, J. Atmos. Sol.-Terr. Phys. 64, 697-705.
  • Lu, G., X. Pi, A.D. Richmond and R.G. Roble, 1998, Variations of total electron content during geomagnetic disturbances: A model/observation comparison, Geophys. Res. Lett. 25, 3, 253-256.
  • Mannucci, A.J., B.D. Wilson, D.N. Yuan, C.H. Ho, U.J. Lindqwister and T.F. Runge, 1998, A global mapping technique for GPS-derived ionospheric total electron content measurements, Radio Science 33, 3, 565-582.
  • Meza, A., M.A. Van Zele, C. Brunini and I.R. Cabassi, 2005, Vertical total electron content and geomagnetic perturbations at mid- and sub-auroral southern latitudes during geomagnetic storms, J. Atmos. Sol.-Terr. Phys. 61, 315-323.
  • Mikhailov, A.V., and M. Forster, 1999, Some F2-layer effects during the January 06-11, 1997 CEDAR storm period as observed with the Millstone Hil incoherent scatter facility, J. Atmos. Sol.-Terr. Phys. 61, 249-261.
  • Pi, X., M. Mendillo, W.J. Hughes, M.J. Buonsanto, D.P Sipler, J. Kelly, Q. Zhou, G. Lu and T.J. Hughes, 2000, Dynamical effects of geomagnetic storms and substorms in the middlelatitude ionosphere: An observational campaign, J. Geophys. Res. 105, A4, 7403-7418.
  • Prolss, G.W., 1993, On explaining the local time variation of the ionospheric storm effects, Ann. Geophys. 11, 1-9.
  • Prolss, G.W., 1995, Ionospheric F-region storms. In: H. Volland (ed.), "Handbook of Atmospheric Electrodynamics", CRC Press, Boca Raton, 2, 195-248.
  • Prolss, G.W., 1997, Magnetic storm associated perturbations of the upper atmosphere. In: B.T. Tsurutani et al. (eds.), "Magnetic Storm", Geophys. Monogr. Series 98, AGU, Washington, D.C., p. 227.
  • Quegan, S., G.J. Bailey, R.J. Moffett, R.A. Heelis, T.J. Fuller-Rowell, D. Rees and R.W. Spiro, 1982, A theoretical study of the distribution of ionization in the high-latitude ionosphere and the plasmasphere: first results on the mid-latitude trough and the light-ion trough, J. Atmos. Sol.-Terr. Phys. 44, 7, 619-640.
  • Rothkaehl, H., F. Jiřiček, S. Šmilauer and M. Förster, 1997, Dynamic changes in the outer ionosphere in the region of the ionospheric trough during an intense magnetic storm, Adv. Space Res. 20, 3, 409-414.
  • Sahai, Y., P.R. Fagundes, F. Becker-Guedes, J.R. Abalde, G. Crowley, X. Pi, K. Igarashi, G.M. Amarante, A.A. Pimenta and J.A. Bittencourt, 2004, Longitudinal differences observed in the ionospheric F-region during the major geomagnetic storm of 31 March 2001, Ann. Geophys. 22, 3221-3229.
  • Shagimuratov, I.I., L.W. Baran, P. Wielgosz, G.A. Yakimova, 2002, The structure of mid- and high-latitude ionosphere during September 1999 storm event obtained from GPS observations, Ann. Geophys. 20, 655-661, http://www.ann-geophys.net/20/655/2002/
  • Shiokawa, K., Y. Ottsuka, T. Ogawa, K. Igarashai, S. Miyazaki, F.J. Rich, A. Saito and Y. Yumoto, 2000, Comprehensive imaging observations of midlatitude ionospheric disturbances during storm time substorms, J. Geophys. Res. 105, A12, 27,067-27,080.
  • Strickland, D.J., R.E. Daniell and J.D. Craven, 2001, Negative ionospheric storm coincident with DE 1 - observed thermospheric disturbance on October 14, 1981, J. Geophys. Res. 106, A10, 21,049-21,062.
  • Tsagouri, I., A. Belehaki, G. Moraitis and H. Mavromichalaki, 2000, Positive and negative ionospheric disturbances at middle latitudes during geomagnetic storms, Geophys. Res. Lett. 27, 21, 3579-3582.
  • Tulunay, Y., I. Stanislawska and H. Rothkaehl, 2003, Revisiting the Ariel trough work for
  • HF telecommunication purposes, Cosmic Res. J. 41, 4, 319-331.
  • Werner, S., and G.W. Prolss, 1997, The position of the ionospheric trough as a function of local time and magnetic activity, Adv. Space Res. 20, 9, 1717-1722.
  • Wielgosz, P., L.W. Baran, I.I. Shagimuratov and M.V. Aleshnikova, 2004, Latitudinal variations of TEC over Europe obtained using GPS observation, Ann. Geophys. 22, 405-415, http://www.ann-geophys.net/22/405/2004/
  • Yizengaw, E., E.A. Essex and R. Birsa, 2004, The Southern Hemisphere and equatorial regionionization response for a 22 September 1999 severe magnetic storm, Ann. Geophys. 22, 2765-2773, http://www.ann-geophys.net/22/2765/2004/
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0021-0055
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