Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/13570
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dc.date.accessioned2020-04-29T06:17:23Z-
dc.date.available2020-04-29T06:17:23Z-
dc.date.issued2020-04-
dc.identifier.urihttp://hdl.handle.net/2122/13570-
dc.description.abstractA statistical analysis of Loss of Lock (LoL) over Brazil throughout the 24th solar cycle is performed. Four geodetic GPS dual-frequency (L1, L2) receivers, deployed at different geographic latitudes ranging from about 25° to 2° South in the eastern part of the country, are used to investigate the LoL dependence on time of the day, season, solar and geomagnetic activity. The results of the analysis show that LoL is most likely in the post-sunset hours during summer and equinox, especially within the southern crest of the Equatorial Ionospheric Anomaly (EIA), in a region between about 10°S and 25°S of geographic latitude, matching the typical behaviour of scintillation over Brazil. This is confirmed by the correlation found between the relative occurrence of LoL (LoL (%)) and the Rate Of TEC Index (ROTI), used as a proxy of scintillation index and calculated for each receivers along the entire period of investigation. The LoL (%) for given solar and geomagnetic indices show some correlation with increasing the severity of the index. This correlation is strongest in the area of the southern crest of the EIA, while there is little to no apparent impact closer to the equator, depending on the index. LoL (%) increases with increasing geomagnetic disturbances, varying between ~1% and ~10% for AE ranged between 400 and 1200 nT, and exceeding 3% when Dst is around −100 nT, both related to moderate-severely disturbed conditions.en_US
dc.language.isoEnglishen_US
dc.publisher.nameElsevieren_US
dc.relation.ispartofAdvances in Space Researchen_US
dc.relation.ispartofseries2/66 (2020)en_US
dc.subjectGPS Loss of Lock, Equatorial Ionosphereen_US
dc.subjectscintillationen_US
dc.titleGPS loss of lock statistics over Brazil during the 24th solar cycleen_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber219-225en_US
dc.identifier.doi10.1016/j.asr.2020.03.041en_US
dc.description.obiettivoSpecifico2A. Fisica dell'alta atmosferaen_US
dc.description.journalTypeJCR Journalen_US
dc.relation.issn0273-1177en_US
dc.contributor.authorDamaceno, Juliana G-
dc.contributor.authorBolmgren, Karl-
dc.contributor.authorBruno, Jon-
dc.contributor.authorDe Franceschi, Giorgiana-
dc.contributor.authorMitchell, Cathryn-
dc.contributor.authorCafaro, Massimo-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italiaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.dept3Department of Electronic and Electrical Engineering, University of Bath-
crisitem.author.orcid0000-0002-6280-6777-
crisitem.author.orcid0000-0001-5456-3894-
crisitem.author.orcid0000-0003-0383-9947-
crisitem.author.orcid0000-0002-3943-6798-
crisitem.author.orcid0000-0003-1118-7109-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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