Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina

Autores
Alfonsi, L.; Spolli, L.; Pezzopane, M.; Romano, V.; Zuccheretti, E.; De. Franceschi, G.; Cabrera, Miguel Angel; Ezquer, Rodolfo Gerardo
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We analyze data recorded from October 2010 to September 2011, during the ascending phase of the 24th solar cycle, from an Advanced Ionospheric Sounder-Istituto Nazionale di Geofisica e Vulcanologia ionosonde and a GPS Ionospheric Scintillation and total electron content (TEC) monitor scintillation receiver, colocated at low latitude in the Southern American longitudinal sector (Tucumán, 26.9°S, 294.6°E, magnetic latitude 15.5°S,Argentina). The site offers the opportunity to perform spread-F and GPS scintillation statistics of occurrence under the southern crest of the equatorial ionospheric anomaly. Spread-F signatures, classified into four types (strong range spread-F (SSF), range spread-F,frequency spread-F (FSF), and mixed spread-F), the phase and amplitude scintillation index (σΦ and S4, respectively), the TEC, and the rate of TEC parameter, marker of the TEC gradients, that can cause scintillations, are considered. The seasonal behavior results as follows: the occurrence of all four types of spread-F is higher in summer and lower in winter, while the occurrence of scintillations peaks at equinoxes in the postsunset sector and shows a minimum in winter. The correspondence between SSF and scintillations seems to be systematic, and a possible correlation between S4 and FSF peaks is envisaged at the terminator. The investigation focused also on two particular periods, from 12 to 16 March 2011 and from 23 to 29 September 2011, both characterized by the simultaneous presence of SSF signatures and scintillation phenomena, allowing to discuss the role of traveling ionospheric disturbances as a strong candidate causing ionospheric irregularities.
Fil: Alfonsi, L.. Istituto Nazionale Di Geofisica E Vulcanologia; Italia
Fil: Spolli, L.. Istituto Nazionale Di Geofisica E Vulcanologia; Italia
Fil: Pezzopane, M.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Romano, V.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Zuccheretti, E.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: De. Franceschi, G.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Cabrera, Miguel Angel. Universidad Tecnológica Nacional. Facultad Regional Tucuman; Argentina
Fil: Ezquer, Rodolfo Gerardo. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física. Laboratorio de Ionósfera; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina
Materia
Ionosphere (equatorial)
Positioning system
Disturbances
Irregularities
Monitoring
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/77317

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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, ArgentinaAlfonsi, L.Spolli, L.Pezzopane, M.Romano, V.Zuccheretti, E.De. Franceschi, G.Cabrera, Miguel AngelEzquer, Rodolfo GerardoIonosphere (equatorial)Positioning systemDisturbancesIrregularitiesMonitoringhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We analyze data recorded from October 2010 to September 2011, during the ascending phase of the 24th solar cycle, from an Advanced Ionospheric Sounder-Istituto Nazionale di Geofisica e Vulcanologia ionosonde and a GPS Ionospheric Scintillation and total electron content (TEC) monitor scintillation receiver, colocated at low latitude in the Southern American longitudinal sector (Tucumán, 26.9°S, 294.6°E, magnetic latitude 15.5°S,Argentina). The site offers the opportunity to perform spread-F and GPS scintillation statistics of occurrence under the southern crest of the equatorial ionospheric anomaly. Spread-F signatures, classified into four types (strong range spread-F (SSF), range spread-F,frequency spread-F (FSF), and mixed spread-F), the phase and amplitude scintillation index (σΦ and S4, respectively), the TEC, and the rate of TEC parameter, marker of the TEC gradients, that can cause scintillations, are considered. The seasonal behavior results as follows: the occurrence of all four types of spread-F is higher in summer and lower in winter, while the occurrence of scintillations peaks at equinoxes in the postsunset sector and shows a minimum in winter. The correspondence between SSF and scintillations seems to be systematic, and a possible correlation between S4 and FSF peaks is envisaged at the terminator. The investigation focused also on two particular periods, from 12 to 16 March 2011 and from 23 to 29 September 2011, both characterized by the simultaneous presence of SSF signatures and scintillation phenomena, allowing to discuss the role of traveling ionospheric disturbances as a strong candidate causing ionospheric irregularities.Fil: Alfonsi, L.. Istituto Nazionale Di Geofisica E Vulcanologia; ItaliaFil: Spolli, L.. Istituto Nazionale Di Geofisica E Vulcanologia; ItaliaFil: Pezzopane, M.. Istituto Nazionale di Geofisica e Vulcanologia; ItaliaFil: Romano, V.. Istituto Nazionale di Geofisica e Vulcanologia; ItaliaFil: Zuccheretti, E.. Istituto Nazionale di Geofisica e Vulcanologia; ItaliaFil: De. Franceschi, G.. Istituto Nazionale di Geofisica e Vulcanologia; ItaliaFil: Cabrera, Miguel Angel. Universidad Tecnológica Nacional. Facultad Regional Tucuman; ArgentinaFil: Ezquer, Rodolfo Gerardo. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física. Laboratorio de Ionósfera; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; ArgentinaAmerican Geophysical Union2013-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/77317Alfonsi, L.; Spolli, L.; Pezzopane, M.; Romano, V.; Zuccheretti, E.; et al.; Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina; American Geophysical Union; Journal of Geophysical Research; 118; 7; 12-2013; 4483-44830148-0227CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1002/jgra.50378, 2013info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/jgra.50378info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:57:46Zoai:ri.conicet.gov.ar:11336/77317instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:57:47.17CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
title Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
spellingShingle Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
Alfonsi, L.
Ionosphere (equatorial)
Positioning system
Disturbances
Irregularities
Monitoring
title_short Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
title_full Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
title_fullStr Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
title_full_unstemmed Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
title_sort Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina
dc.creator.none.fl_str_mv Alfonsi, L.
Spolli, L.
Pezzopane, M.
Romano, V.
Zuccheretti, E.
De. Franceschi, G.
Cabrera, Miguel Angel
Ezquer, Rodolfo Gerardo
author Alfonsi, L.
author_facet Alfonsi, L.
Spolli, L.
Pezzopane, M.
Romano, V.
Zuccheretti, E.
De. Franceschi, G.
Cabrera, Miguel Angel
Ezquer, Rodolfo Gerardo
author_role author
author2 Spolli, L.
Pezzopane, M.
Romano, V.
Zuccheretti, E.
De. Franceschi, G.
Cabrera, Miguel Angel
Ezquer, Rodolfo Gerardo
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Ionosphere (equatorial)
Positioning system
Disturbances
Irregularities
Monitoring
topic Ionosphere (equatorial)
Positioning system
Disturbances
Irregularities
Monitoring
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv We analyze data recorded from October 2010 to September 2011, during the ascending phase of the 24th solar cycle, from an Advanced Ionospheric Sounder-Istituto Nazionale di Geofisica e Vulcanologia ionosonde and a GPS Ionospheric Scintillation and total electron content (TEC) monitor scintillation receiver, colocated at low latitude in the Southern American longitudinal sector (Tucumán, 26.9°S, 294.6°E, magnetic latitude 15.5°S,Argentina). The site offers the opportunity to perform spread-F and GPS scintillation statistics of occurrence under the southern crest of the equatorial ionospheric anomaly. Spread-F signatures, classified into four types (strong range spread-F (SSF), range spread-F,frequency spread-F (FSF), and mixed spread-F), the phase and amplitude scintillation index (σΦ and S4, respectively), the TEC, and the rate of TEC parameter, marker of the TEC gradients, that can cause scintillations, are considered. The seasonal behavior results as follows: the occurrence of all four types of spread-F is higher in summer and lower in winter, while the occurrence of scintillations peaks at equinoxes in the postsunset sector and shows a minimum in winter. The correspondence between SSF and scintillations seems to be systematic, and a possible correlation between S4 and FSF peaks is envisaged at the terminator. The investigation focused also on two particular periods, from 12 to 16 March 2011 and from 23 to 29 September 2011, both characterized by the simultaneous presence of SSF signatures and scintillation phenomena, allowing to discuss the role of traveling ionospheric disturbances as a strong candidate causing ionospheric irregularities.
Fil: Alfonsi, L.. Istituto Nazionale Di Geofisica E Vulcanologia; Italia
Fil: Spolli, L.. Istituto Nazionale Di Geofisica E Vulcanologia; Italia
Fil: Pezzopane, M.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Romano, V.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Zuccheretti, E.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: De. Franceschi, G.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Cabrera, Miguel Angel. Universidad Tecnológica Nacional. Facultad Regional Tucuman; Argentina
Fil: Ezquer, Rodolfo Gerardo. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física. Laboratorio de Ionósfera; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina
description We analyze data recorded from October 2010 to September 2011, during the ascending phase of the 24th solar cycle, from an Advanced Ionospheric Sounder-Istituto Nazionale di Geofisica e Vulcanologia ionosonde and a GPS Ionospheric Scintillation and total electron content (TEC) monitor scintillation receiver, colocated at low latitude in the Southern American longitudinal sector (Tucumán, 26.9°S, 294.6°E, magnetic latitude 15.5°S,Argentina). The site offers the opportunity to perform spread-F and GPS scintillation statistics of occurrence under the southern crest of the equatorial ionospheric anomaly. Spread-F signatures, classified into four types (strong range spread-F (SSF), range spread-F,frequency spread-F (FSF), and mixed spread-F), the phase and amplitude scintillation index (σΦ and S4, respectively), the TEC, and the rate of TEC parameter, marker of the TEC gradients, that can cause scintillations, are considered. The seasonal behavior results as follows: the occurrence of all four types of spread-F is higher in summer and lower in winter, while the occurrence of scintillations peaks at equinoxes in the postsunset sector and shows a minimum in winter. The correspondence between SSF and scintillations seems to be systematic, and a possible correlation between S4 and FSF peaks is envisaged at the terminator. The investigation focused also on two particular periods, from 12 to 16 March 2011 and from 23 to 29 September 2011, both characterized by the simultaneous presence of SSF signatures and scintillation phenomena, allowing to discuss the role of traveling ionospheric disturbances as a strong candidate causing ionospheric irregularities.
publishDate 2013
dc.date.none.fl_str_mv 2013-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/77317
Alfonsi, L.; Spolli, L.; Pezzopane, M.; Romano, V.; Zuccheretti, E.; et al.; Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina; American Geophysical Union; Journal of Geophysical Research; 118; 7; 12-2013; 4483-4483
0148-0227
CONICET Digital
CONICET
url http://hdl.handle.net/11336/77317
identifier_str_mv Alfonsi, L.; Spolli, L.; Pezzopane, M.; Romano, V.; Zuccheretti, E.; et al.; Comparative analysis of spread-F signature and GPS scintillation ocurrences at Tucuman, Argentina; American Geophysical Union; Journal of Geophysical Research; 118; 7; 12-2013; 4483-4483
0148-0227
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1002/jgra.50378, 2013
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/jgra.50378
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432