Variations of foF2 and GPS total electron content over the Antarctic sector
- Autores
- Mosert, M.; McKinnell, L. A.; Gende, Mauricio; Brunini, Claudio Antonio; Araujo, J.; Ezquer, R. G.; Cabrera, M.
- Año de publicación
- 2011
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- This paper presents a preliminary analysis of the variations of the critical frequency of the F2 region (foF2) and the total electron content (TEC) derived from Global Positioning System (GPS) data. Hourly foF2 values were scaled from ionograms recorded at San Martin (68.1°S, 293.0°E) and the TEC values were derived from GPS observations at O'Higgins (63.3°S, 302.5 °E). The database includes measurements obtained under different seasonal and solar activity conditions. The study shows that the daily peak of foF2 occurs around local noon in winter and fall, and in spring a secondary peak is observed around midnight. In summer (January) foF2 reaches its minimum value around the noon sector while the maximum in the diurnal variation of foF2 is located in a time sector close to midnight. This behaviour is observed at low and high solar activity. The semiannual anomaly appears around noon at high and low solar activity and the winter anomaly is not observed. The effect of the solar activity is generally observed in every season. The analysis of the GPS TEC measurements in the same region indicates that the diurnal, seasonal and solar activity variations are similar to those observed in the foF2 values. An analysis of the performance of the IRI model to predict foF2 is also shown using the two IRI options (URSI and CCIR). The comparisons between the experimental values and the IRI predictions show some discrepancies.
Facultad de Ciencias Astronómicas y Geofísicas - Materia
-
Ciencias Astronómicas
GPS TEC
High latitude
Ionosphere
IRI
foF2 - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/83679
Ver los metadatos del registro completo
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Variations of foF2 and GPS total electron content over the Antarctic sectorMosert, M.McKinnell, L. A.Gende, MauricioBrunini, Claudio AntonioAraujo, J.Ezquer, R. G.Cabrera, M.Ciencias AstronómicasGPS TECHigh latitudeIonosphereIRIfoF2This paper presents a preliminary analysis of the variations of the critical frequency of the F<SUB>2</SUB> region (f<SUB>o</SUB>F<SUB>2</SUB>) and the total electron content (TEC) derived from Global Positioning System (GPS) data. Hourly f<SUB>o</SUB>F<SUB>2</SUB> values were scaled from ionograms recorded at San Martin (68.1°S, 293.0°E) and the TEC values were derived from GPS observations at O'Higgins (63.3°S, 302.5 °E). The database includes measurements obtained under different seasonal and solar activity conditions. The study shows that the daily peak of f<SUB>o</SUB>F<SUB>2</SUB> occurs around local noon in winter and fall, and in spring a secondary peak is observed around midnight. In summer (January) f<SUB>o</SUB>F<SUB>2</SUB> reaches its minimum value around the noon sector while the maximum in the diurnal variation of f<SUB>o</SUB>F<SUB>2</SUB> is located in a time sector close to midnight. This behaviour is observed at low and high solar activity. The semiannual anomaly appears around noon at high and low solar activity and the winter anomaly is not observed. The effect of the solar activity is generally observed in every season. The analysis of the GPS TEC measurements in the same region indicates that the diurnal, seasonal and solar activity variations are similar to those observed in the f<SUB>o</SUB>F<SUB>2</SUB> values. An analysis of the performance of the IRI model to predict f<SUB>o</SUB>F<SUB>2</SUB> is also shown using the two IRI options (URSI and CCIR). The comparisons between the experimental values and the IRI predictions show some discrepancies.Facultad de Ciencias Astronómicas y Geofísicas2011info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf327-333http://sedici.unlp.edu.ar/handle/10915/83679enginfo:eu-repo/semantics/altIdentifier/issn/1343-8832info:eu-repo/semantics/altIdentifier/doi/10.5047/eps.2011.01.006info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:15:55Zoai:sedici.unlp.edu.ar:10915/83679Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:15:55.884SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Variations of foF2 and GPS total electron content over the Antarctic sector |
title |
Variations of foF2 and GPS total electron content over the Antarctic sector |
spellingShingle |
Variations of foF2 and GPS total electron content over the Antarctic sector Mosert, M. Ciencias Astronómicas GPS TEC High latitude Ionosphere IRI foF2 |
title_short |
Variations of foF2 and GPS total electron content over the Antarctic sector |
title_full |
Variations of foF2 and GPS total electron content over the Antarctic sector |
title_fullStr |
Variations of foF2 and GPS total electron content over the Antarctic sector |
title_full_unstemmed |
Variations of foF2 and GPS total electron content over the Antarctic sector |
title_sort |
Variations of foF2 and GPS total electron content over the Antarctic sector |
dc.creator.none.fl_str_mv |
Mosert, M. McKinnell, L. A. Gende, Mauricio Brunini, Claudio Antonio Araujo, J. Ezquer, R. G. Cabrera, M. |
author |
Mosert, M. |
author_facet |
Mosert, M. McKinnell, L. A. Gende, Mauricio Brunini, Claudio Antonio Araujo, J. Ezquer, R. G. Cabrera, M. |
author_role |
author |
author2 |
McKinnell, L. A. Gende, Mauricio Brunini, Claudio Antonio Araujo, J. Ezquer, R. G. Cabrera, M. |
author2_role |
author author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Astronómicas GPS TEC High latitude Ionosphere IRI foF2 |
topic |
Ciencias Astronómicas GPS TEC High latitude Ionosphere IRI foF2 |
dc.description.none.fl_txt_mv |
This paper presents a preliminary analysis of the variations of the critical frequency of the F<SUB>2</SUB> region (f<SUB>o</SUB>F<SUB>2</SUB>) and the total electron content (TEC) derived from Global Positioning System (GPS) data. Hourly f<SUB>o</SUB>F<SUB>2</SUB> values were scaled from ionograms recorded at San Martin (68.1°S, 293.0°E) and the TEC values were derived from GPS observations at O'Higgins (63.3°S, 302.5 °E). The database includes measurements obtained under different seasonal and solar activity conditions. The study shows that the daily peak of f<SUB>o</SUB>F<SUB>2</SUB> occurs around local noon in winter and fall, and in spring a secondary peak is observed around midnight. In summer (January) f<SUB>o</SUB>F<SUB>2</SUB> reaches its minimum value around the noon sector while the maximum in the diurnal variation of f<SUB>o</SUB>F<SUB>2</SUB> is located in a time sector close to midnight. This behaviour is observed at low and high solar activity. The semiannual anomaly appears around noon at high and low solar activity and the winter anomaly is not observed. The effect of the solar activity is generally observed in every season. The analysis of the GPS TEC measurements in the same region indicates that the diurnal, seasonal and solar activity variations are similar to those observed in the f<SUB>o</SUB>F<SUB>2</SUB> values. An analysis of the performance of the IRI model to predict f<SUB>o</SUB>F<SUB>2</SUB> is also shown using the two IRI options (URSI and CCIR). The comparisons between the experimental values and the IRI predictions show some discrepancies. Facultad de Ciencias Astronómicas y Geofísicas |
description |
This paper presents a preliminary analysis of the variations of the critical frequency of the F<SUB>2</SUB> region (f<SUB>o</SUB>F<SUB>2</SUB>) and the total electron content (TEC) derived from Global Positioning System (GPS) data. Hourly f<SUB>o</SUB>F<SUB>2</SUB> values were scaled from ionograms recorded at San Martin (68.1°S, 293.0°E) and the TEC values were derived from GPS observations at O'Higgins (63.3°S, 302.5 °E). The database includes measurements obtained under different seasonal and solar activity conditions. The study shows that the daily peak of f<SUB>o</SUB>F<SUB>2</SUB> occurs around local noon in winter and fall, and in spring a secondary peak is observed around midnight. In summer (January) f<SUB>o</SUB>F<SUB>2</SUB> reaches its minimum value around the noon sector while the maximum in the diurnal variation of f<SUB>o</SUB>F<SUB>2</SUB> is located in a time sector close to midnight. This behaviour is observed at low and high solar activity. The semiannual anomaly appears around noon at high and low solar activity and the winter anomaly is not observed. The effect of the solar activity is generally observed in every season. The analysis of the GPS TEC measurements in the same region indicates that the diurnal, seasonal and solar activity variations are similar to those observed in the f<SUB>o</SUB>F<SUB>2</SUB> values. An analysis of the performance of the IRI model to predict f<SUB>o</SUB>F<SUB>2</SUB> is also shown using the two IRI options (URSI and CCIR). The comparisons between the experimental values and the IRI predictions show some discrepancies. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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dc.identifier.none.fl_str_mv |
http://sedici.unlp.edu.ar/handle/10915/83679 |
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http://sedici.unlp.edu.ar/handle/10915/83679 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/issn/1343-8832 info:eu-repo/semantics/altIdentifier/doi/10.5047/eps.2011.01.006 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
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openAccess |
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http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
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