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Evaluation of the STORM model storm-time corrections for middle latitude
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SYSNO ASEP 0348460 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Evaluation of the STORM model storm-time corrections for middle latitude Tvůrce(i) Burešová, Dalia (UFA-U) RID, ORCID
McKinnell, L.- A. (ZA)
Šindelářová, Tereza (UFA-U) RID, ORCID
de la Morena, B. A. (ES)Zdroj.dok. Advances in Space Research. - : Elsevier - ISSN 0273-1177
Roč. 46, č. 8 (2010), s. 1039-1046Poč.str. 8 s. Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova Ionosphere ; Geomagnetic storms ; STORM model ; International Reference Ionosphere (IRI) Vědní obor RIV DG - Vědy o atmosféře, meteorologie CEP GA205/08/1356 GA ČR - Grantová agentura ČR 1QS300120506 GA AV ČR - Akademie věd CEZ AV0Z30420517 - UFA-U, BC-A (2005-2011) UT WOS 000282675400009 DOI 10.1016/j.asr.2010.06.007 Anotace This paper presents results from the Storm-Time Ionospheric Correction Model (STORM) validation for selected Northern and Southern Hemisphere middle latitude locations. This validation included data from some ionospheric stations (e.g., Pruhonice, El Arenosillo) that were not considered in the development or previous validations of the model. Hourly values of the F2 layer critical frequency, foF2, measured for 5–7 days during the main and recovery phases of each selected storm were compared with the predicted IRI 2007 foF2 with the STORM model option activated. To perform a detailed comparison the correlation coefficient, the RMSE, and the percentage improvement were calculated. Results of the comparative analysis show that the STORM model captures more effectively the negative phases of the summer ionospheric storms, while electron density enhancement during winter storms and the changeover of the different storm phases is reproduced with less accuracy. Pracoviště Ústav fyziky atmosféry Kontakt Kateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019 Rok sběru 2011
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