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Seasonal Variations of Mid-Latitude Ionospheric Trough Structure Observed with DEMETER and COSMIC

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The mid-latitude ionospheric trough is a depleted region of ionospheric plasma observed in the topside ionosphere. Its behavior can provide useful information about the magnetospheric dynamics, since its existence is sensitive to magnetospherically induced motions. Midlatitude trough is mainly a night-time phenomenon. Both, its general features and detailed characteristics strongly depend on the level of geomagnetic disturbances, time of the day, season, and the solar cycle, among others. Although many studies provide basic information about general characteristics of the main ionospheric trough structure, an accurate prediction of the trough behavior in specific events is still understood poorly. The paper presents the mid-latitude trough characteristics with regard to the geomagnetic longitude and season during a solar activity minimum, as based on the DEMETER in situ satellite measurements and the data retrieved from FORMOSAT-3/COSMIC radio occultation measurements.
Czasopismo
Rocznik
Strony
2734--2747
Opis fizyczny
Bibliogr. 15 poz.
Twórcy
  • Space Research Centre of Polish Academy of Sciences, Warsaw, Poland
  • Space Research Centre of Polish Academy of Sciences, Warsaw, Poland
autor
  • Space Research Centre of Polish Academy of Sciences, Warsaw, Poland
Bibliografia
  • Aladjev, G.A., O.V. Evstaev, V.S. Mingalev, G.I. Mingaleva, E.D. Tereshchenko, and B.Z. Khudukon (2001), Interpretation of ionospheric F-region structures in the vicinity of ionization trough observed by satellite radio tomography, Ann. Geophys. 19, 1, 25-36.
  • Clilverd, M.A., N.R. Thomson, and A.J. Smith (1995), The effect of the mid-latitude ionospheric trough on whistler mode ducting during magnetic storm, J. Atmos. Terr. Phys. 57, 8, 945-954, DOI: 10.1016/0021-9169(94)00083-Z.
  • He, M., L. Liu, W. Wan, and B. Zhao (2011), A study on the night-time midlatitude ionospheric trough, J. Geophys. Res. 116, A5, A05315, DOI: 10.1029/ 2010JA016252.
  • Horvath, I., and E.A. Essex (2003), The Weddell Sea Anomaly observed with the Topex satellite data, J. Atmos. Sol. Terr. Phys. 65, 6, 693-706, DOI: 10.1016/S1364-6826(03)00083-X.
  • Karpachev, A.T. (2003), The dependence of the main ionospheric trough shape on longitude, altitude, season, local time, and solar and magnetic activity, Geomagn. Aeron. 43, 2, 239-251.
  • Lebreton, J.-P., S. Stverak, P. Travnicek, M. Maksimovic, D. Klinge, S. Merikallio, D. Lagoutte, B. Poirier, P.-L. Blelly, Z. Kozacek, and M. Salaquarda (2006), The ISL Langmuir probe experiment processing onboard DEMETER: Scientific objectives, description and first results, Planet. Space Sci. 54, 5, 472-486, DOI: 10.1016/j.pss.2005.10.017.
  • Mallis, M., and E. Essex (1993), Diurnal and seasonal variability of the southernhemisphere main ionospheric trough from differentialphase measurements, J. Atmos. Terr. Phys. 55, 7, 1021-1037, DOI: 10.1016/0021-9169(93) 90095-G.
  • Moffett, R.J., and S. Quegan (1983), The midlatitude trough in the electron concentration of the ionospheric Flayer: A review of observations and modeling, J. Atmos. Terr. Phys. 45, 5, 315-343, DOI: 10.1016/S0021-9169(83)80038-5.
  • Muldrew, D.B. (1965), Flayer ionization trough deduced from Alouette data, J. Geophys. Res. 70, 11, 2635-2650, DOI: 10.1029/JZ070i011p02635.
  • Rothkaehl, H., F. Jiricek, J. Smilauer, and M. Förster (1997), Dynamic changes in the outer ionosphere in the region of the ionospheric trough during and intense magnetic storm, Adv. Space Res. 20, 3, 409-414, DOI: 10.1016/ S0273-1177(97)00701-1.
  • Spiro, R.W. (1978), Ion convection and the formation of the midlatitude F region ionization trough, J. Geophys. Res. 83, A9, 4255-4264, DOI: 10.1029/ JA083iA09p04255.
  • Werner, S., and G.W. Prölss (1997), The position of the ionospheric trough as a function of local time and magnetic activity, Adv. Space Res. 20, 9, 1717- 1722, DOI: 10.1016/S0273-1177(97)00578-4.
  • Whalen, J.A. (1989), The daytime F layer trough and its relation to ionosphericmagnetospheric convection, J. Geophys. Res. 94, A12, 17169-17184, DOI: 10.1029/JA094iA12p17169.
  • Yizengaw, E., H. Wei, M.B. Moldwin, D. Galvan, L. Mandrake, A. Mannucci, and X. Pi (2005), The correlation between mid-latitude trough and the plasmapause, Geophys. Res. Lett. 32, 10, L10102, DOI: 10.1029/2005GL022954.
  • Zaalov, N.Y., H. Rothkaehl, A.J. Stocker, and E.M. Warrington (2013), Comparison between HF propagation and DEMETER satellite measurements within the mid-latitude trough, Adv. Space Res. 52, 5, 781-790, DOI: 10.1016/j.asr. 2013.05.023.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-ee7f6d72-569a-477b-ab3d-d9fb8e46d299
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