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dc.contributor.author Korenkov, Y. N.
dc.contributor.author Klimenko, V. V.
dc.contributor.author Klimenko, M. V.
dc.contributor.author Bessarab, F. S.
dc.contributor.author Korenkova, N. A.
dc.contributor.author Ratovsky, K. G.
dc.contributor.author Chernigovskaya, M. A.
dc.contributor.author Shcherbakov, A. A.
dc.contributor.author Sahai, Y.
dc.contributor.author Fagundes, P. R.
dc.contributor.author De Jesus, R.
dc.contributor.author De Abreu, A. J.
dc.contributor.author Cóndor, P.
dc.date.accessioned 2018-07-23T13:13:05Z
dc.date.available 2018-07-23T13:13:05Z
dc.date.issued 2012-10-09
dc.identifier.citation Korenkov, Y. N., Klimenko, V. V., Klimenko, M. V., Bessarab, F. S., Korenkova, N. A., Ratovsky, K. G., ... Cóndor, P. (2012). The global thermospheric and ionospheric response to the 2008 minor sudden stratospheric warming event.==$Journal of Geophysical Research: Space Physics, 117$==(A10), A10309. https://doi.org/10.1029/2012JA018018 es_ES
dc.identifier.govdoc index-oti2018
dc.identifier.uri http://hdl.handle.net/20.500.12816/2021
dc.description.abstract This paper presents a study of thermospheric and ionospheric response to the 2008 minor sudden stratospheric warming (SSW) event. This period was characterized by low solar and geomagnetic activity. The study was performed using the Global Self-consistent Model of Thermosphere, Ionosphere, and Protonosphere (GSM TIP). Model results were compared with ionosonde data from Irkutsk, Kaliningrad, Sao Jose dos Campos, and Jicamarca. The SSW event was modeled by specifying the temperature and density perturbations at the lower boundary of the GSM TIP (80 km altitude). GSM TIP simulation allowed the reproduction of the lower thermosphere temperature disturbances (the occurrence of the quasi-wave 1 structure at 80–130 km altitude with a vertical scale of 40 km), the negative response of F2 region electron density and the positive response of electron temperature at 300 km during the 2008 minor SSW event. The main formation mechanism of the global ionospheric response is due to the disturbances (decrease) in the n(O)/n(N2) ratio. The change in zonal electric field is another important mechanism of the ionospheric response at low latitudes. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher American Geophysical Union es_ES
dc.relation.ispartof urn:issn:2169-9380
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.subject Electric field es_ES
dc.subject Ionosphere es_ES
dc.subject Sudden stratospheric warming es_ES
dc.subject Thermosphere es_ES
dc.title The global thermospheric and ionospheric response to the 2008 minor sudden stratospheric warming event es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.01 es_ES
dc.identifier.journal Journal of Geophysical Research: Space Physics es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi https://doi.org/10.1029/2012JA018018 es_ES

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