Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps
- Autores
- Meza, A.; Natali, Maria Paula; Fernandez, Laura Isabel
- Año de publicación
- 2012
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Our work is focused on the analysis of seasonal and semiannual ionospheric anomalies using vertical total electron content (VTEC) measurements obtained by the International GNSS Service (IGS). For this study we use principal component analysis (PCA) and wavelet transform (WT) because both numerical tools allow us to isolate principal components of the VTEC variability as much spatially as temporally. The IGS VTEC maps are reorganized, and from each daily global data set, two maps were constructed: one at 12:00 LT and the other at 22:00 LT. From these two series of VTEC maps covering the period 1999–2009 for each local time, we found that the semiannual anomaly is globally recorded at noon, especially at mid and low geomagnetic latitudes, and its amplitude has a close relationship with the solar activity, and at night this anomaly is recorded during high solar activity and the larger values are located in the South American region. The values of VTEC at the March equinox exceed that of the September equinox, especially during high solar activity; the winter anomaly is recorded at noon near the geomagnetic poles region, and the effect is more important during high solar activity. At night this anomaly is present during the ascending and descending phases and minimum of the solar cycle. Thus, the night winter anomaly effect is clearly evidenced from our results.
Fil: Meza, A.. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Natali, Maria Paula. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Fernandez, Laura Isabel. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Materia
-
Principal Component Analysis
Global IGS Vtec maps
anomalies
winter and semiannual anomalies - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/241667
Ver los metadatos del registro completo
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Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service mapsMeza, A.Natali, Maria PaulaFernandez, Laura IsabelPrincipal Component AnalysisGlobal IGS Vtec mapsanomalieswinter and semiannual anomalieshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Our work is focused on the analysis of seasonal and semiannual ionospheric anomalies using vertical total electron content (VTEC) measurements obtained by the International GNSS Service (IGS). For this study we use principal component analysis (PCA) and wavelet transform (WT) because both numerical tools allow us to isolate principal components of the VTEC variability as much spatially as temporally. The IGS VTEC maps are reorganized, and from each daily global data set, two maps were constructed: one at 12:00 LT and the other at 22:00 LT. From these two series of VTEC maps covering the period 1999–2009 for each local time, we found that the semiannual anomaly is globally recorded at noon, especially at mid and low geomagnetic latitudes, and its amplitude has a close relationship with the solar activity, and at night this anomaly is recorded during high solar activity and the larger values are located in the South American region. The values of VTEC at the March equinox exceed that of the September equinox, especially during high solar activity; the winter anomaly is recorded at noon near the geomagnetic poles region, and the effect is more important during high solar activity. At night this anomaly is present during the ascending and descending phases and minimum of the solar cycle. Thus, the night winter anomaly effect is clearly evidenced from our results.Fil: Meza, A.. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Natali, Maria Paula. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Fernandez, Laura Isabel. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaAmerican Geophysical Union2012-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/zipapplication/pdfhttp://hdl.handle.net/11336/241667Meza, A.; Natali, Maria Paula; Fernandez, Laura Isabel; Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps; American Geophysical Union; Journal of Geophysical Research; 117; A1; 1-2012; 1-100148-0227CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2011JA016882info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JA016882info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:23:15Zoai:ri.conicet.gov.ar:11336/241667instacron: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:34982025-10-22 11:23:15.996CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| title |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| spellingShingle |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps Meza, A. Principal Component Analysis Global IGS Vtec maps anomalies winter and semiannual anomalies |
| title_short |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| title_full |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| title_fullStr |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| title_full_unstemmed |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| title_sort |
Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps |
| dc.creator.none.fl_str_mv |
Meza, A. Natali, Maria Paula Fernandez, Laura Isabel |
| author |
Meza, A. |
| author_facet |
Meza, A. Natali, Maria Paula Fernandez, Laura Isabel |
| author_role |
author |
| author2 |
Natali, Maria Paula Fernandez, Laura Isabel |
| author2_role |
author author |
| dc.subject.none.fl_str_mv |
Principal Component Analysis Global IGS Vtec maps anomalies winter and semiannual anomalies |
| topic |
Principal Component Analysis Global IGS Vtec maps anomalies winter and semiannual anomalies |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Our work is focused on the analysis of seasonal and semiannual ionospheric anomalies using vertical total electron content (VTEC) measurements obtained by the International GNSS Service (IGS). For this study we use principal component analysis (PCA) and wavelet transform (WT) because both numerical tools allow us to isolate principal components of the VTEC variability as much spatially as temporally. The IGS VTEC maps are reorganized, and from each daily global data set, two maps were constructed: one at 12:00 LT and the other at 22:00 LT. From these two series of VTEC maps covering the period 1999–2009 for each local time, we found that the semiannual anomaly is globally recorded at noon, especially at mid and low geomagnetic latitudes, and its amplitude has a close relationship with the solar activity, and at night this anomaly is recorded during high solar activity and the larger values are located in the South American region. The values of VTEC at the March equinox exceed that of the September equinox, especially during high solar activity; the winter anomaly is recorded at noon near the geomagnetic poles region, and the effect is more important during high solar activity. At night this anomaly is present during the ascending and descending phases and minimum of the solar cycle. Thus, the night winter anomaly effect is clearly evidenced from our results. Fil: Meza, A.. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina Fil: Natali, Maria Paula. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina Fil: Fernandez, Laura Isabel. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
| description |
Our work is focused on the analysis of seasonal and semiannual ionospheric anomalies using vertical total electron content (VTEC) measurements obtained by the International GNSS Service (IGS). For this study we use principal component analysis (PCA) and wavelet transform (WT) because both numerical tools allow us to isolate principal components of the VTEC variability as much spatially as temporally. The IGS VTEC maps are reorganized, and from each daily global data set, two maps were constructed: one at 12:00 LT and the other at 22:00 LT. From these two series of VTEC maps covering the period 1999–2009 for each local time, we found that the semiannual anomaly is globally recorded at noon, especially at mid and low geomagnetic latitudes, and its amplitude has a close relationship with the solar activity, and at night this anomaly is recorded during high solar activity and the larger values are located in the South American region. The values of VTEC at the March equinox exceed that of the September equinox, especially during high solar activity; the winter anomaly is recorded at noon near the geomagnetic poles region, and the effect is more important during high solar activity. At night this anomaly is present during the ascending and descending phases and minimum of the solar cycle. Thus, the night winter anomaly effect is clearly evidenced from our results. |
| publishDate |
2012 |
| dc.date.none.fl_str_mv |
2012-01 |
| 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 |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/241667 Meza, A.; Natali, Maria Paula; Fernandez, Laura Isabel; Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps; American Geophysical Union; Journal of Geophysical Research; 117; A1; 1-2012; 1-10 0148-0227 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/241667 |
| identifier_str_mv |
Meza, A.; Natali, Maria Paula; Fernandez, Laura Isabel; Analysis of the winter and semiannual ionospheric anomalies in 1999?2009 based on GPS global International GNSS Service maps; American Geophysical Union; Journal of Geophysical Research; 117; A1; 1-2012; 1-10 0148-0227 CONICET Digital CONICET |
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eng |
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eng |
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American Geophysical Union |
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American Geophysical Union |
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