دورية أكاديمية

Low-latitude equinoctial spread-F occurrence at different longitude sectors under low solar activity

التفاصيل البيبلوغرافية
العنوان: Low-latitude equinoctial spread-F occurrence at different longitude sectors under low solar activity
المؤلفون: Pezzopane, M., Zuccheretti, E., Abadi, P., de Abreu, A. J., de Jesus, R., Fagundes, P. R., Supnithi, P., Rungraengwajiake, S., Nagatsuma, T., Tsugawa, T., Cabrera, Miguel Angel, Ezquer, Rodolfo Gerardo
بيانات النشر: Copernicus Publications
المجموعة: CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
مصطلحات موضوعية: IONOSPHERE, EQUATORIAL IONOSPHERE, IONOSPHERIC IRREGULARITIES, WAVE PROPAGATION, https://purl.org/becyt/ford/1.5Test, https://purl.org/becyt/ford/1Test
الوصف: We present the results of a comparative study of spread-F signatures over five low-latitude sites: Chiangmai (CGM; 18.8° N, 98.9° E, mag. Lat. 8.8° N), Thailand; Tanjungsari (TNJ; 6.9° S, 107.6° E, mag. Lat. 16.9° S), Indonesia; Palmas (PAL; 10.2° S, 311.8° E, mag. Lat. 0.9° S) and São José Dos Campos (SJC; 23.2° S, 314.1° E, mag. Lat. 14.0° S), Brazil; and Tucumán (TUC; 26.9° S, 294.6° E, mag. Lat. 16.8° S), Argentina. The investigation was based on simultaneous ionograms recorded by an FMCW (frequency-modulated continuous-wave) at CGM, an IPS-71 (digital ionosonde from KEL aerospace) at TNJ, a CADI (Canadian Advanced Digital Ionosonde) at PAL and SJC, and an AIS-INGV (Advanced Ionospheric Sounder – Istituto Nazionale di Geofisica e Vulcanologia) at TUC, during the equinoctial periods March–April (R12 = 2.0 and R12 = 2.2) and September–October (R12 = 6.1 and R12 = 7.0) 2009, for very low solar activity. Spread-F signatures were categorized into two types: the range spread-F (RSF) and the frequency spread-F (FSF). The study confirms that the dynamics and the physical processes responsible for these phenomena are actually complicated. In fact, the features that arise from the investigation are different, depending on both the longitude sector and on the hemisphere. For instance, TUC, under the southern crest of the ionospheric equatorial ionization anomaly (EIA), shows a predominance of RSF signatures, while both SJC, under the southern crest of EIA but in a different longitude sector, and CGM, under the northern crest of EIA, show a predominance of FSF signatures. Moreover, the spread-F occurrence over the longitude sector that includes CGM and TNJ is significantly lower than the spread-F occurrence over the longitude sector of PAL, SJC, and TUC. ; Fil: Pezzopane, M. Istituto Nazionale Di Geofisica E Vulcanologia; Italia; ; Fil: Zuccheretti, E. Istituto Nazionale Di Geofisica E Vulcanologia; Italia; ; Fil: Abadi, P. Indonesian National Institute of Aeronautics and Space. Space Science Center. Division of ...
نوع الوثيقة: article in journal/newspaper
وصف الملف: application/pdf
اللغة: English
تدمد: 0992-7689
1432-0576
العلاقة: info:eu-repo/semantics/altIdentifier/url/http://www.ann-geophys.net/31/153/2013/angeo-31-153-2013.pdfTest; http://hdl.handle.net/11336/1576Test; Pezzopane, M.; Zuccheretti, E.; Abadi, P.; de Abreu, A. J.; de Jesus, R.; et al.; Low-latitude equinoctial spread-F occurrence at different longitude sectors under low solar activity; Copernicus Publications; Annales Geophysicae; 31; 5-2-2013; 153-162
الإتاحة: https://doi.org/10.5194/angeo-31-153-2013Test
http://hdl.handle.net/11336/1576Test
حقوق: info:eu-repo/semantics/openAccess ; https://creativecommons.org/licenses/by-nc-sa/2.5/arTest/
رقم الانضمام: edsbas.9A7E46DA
قاعدة البيانات: BASE