Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms
The effect of geomagnetic storms on the mid-high latitude F2 region is studied. For that, foF2 data from four Antarctic stations were analyzed during three intense magnetic storms occurred in high solar activity (years 2002 and 2003). In general, negative storm effects irrespective of the local time...
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ftconicet:oai:ri.conicet.gov.ar:11336/67044 2023-10-09T21:46:57+02:00 Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms Mansilla, Gustavo Adolfo application/pdf http://hdl.handle.net/11336/67044 eng eng Bentham Open info:eu-repo/semantics/altIdentifier/url/http://benthamopen.com/ABSTRACT/TOASCJ-11-16 info:eu-repo/semantics/altIdentifier/doi/10.2174/1874282301711010016 http://hdl.handle.net/11336/67044 Mansilla, Gustavo Adolfo; Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms; Bentham Open; The Open Atmospheric Science Journal; 11; 1; 5-2017; 16-28 1874-2823 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Geomagnetic Storms Ionosphere Mid-High Latitudes https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.2174/1874282301711010016 2023-09-24T19:22:32Z The effect of geomagnetic storms on the mid-high latitude F2 region is studied. For that, foF2 data from four Antarctic stations were analyzed during three intense magnetic storms occurred in high solar activity (years 2002 and 2003). In general, negative storm effects irrespective of the local time were observed during the first part of the storms (main phase). Negative effects were also observed more often than positive effects during the first part of the recovery phase, which seems to indicate almost no longitudinal dependence in this stage of the storm. The negative effects frequently changed to positive during the last stage of the recovery. Several physical mechanisms were operative during the different stages of the storms. Fil: Mansilla, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina Article in Journal/Newspaper Antarc* Antarctic CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Argentina Tucumán ENVELOPE(-63.200,-63.200,-64.683,-64.683) Gustavo ENVELOPE(-62.917,-62.917,-64.833,-64.833) Mansilla ENVELOPE(-67.167,-67.167,-66.383,-66.383) The Open Atmospheric Science Journal 11 1 16 28 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
Geomagnetic Storms Ionosphere Mid-High Latitudes https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
Geomagnetic Storms Ionosphere Mid-High Latitudes https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Mansilla, Gustavo Adolfo Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
topic_facet |
Geomagnetic Storms Ionosphere Mid-High Latitudes https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
The effect of geomagnetic storms on the mid-high latitude F2 region is studied. For that, foF2 data from four Antarctic stations were analyzed during three intense magnetic storms occurred in high solar activity (years 2002 and 2003). In general, negative storm effects irrespective of the local time were observed during the first part of the storms (main phase). Negative effects were also observed more often than positive effects during the first part of the recovery phase, which seems to indicate almost no longitudinal dependence in this stage of the storm. The negative effects frequently changed to positive during the last stage of the recovery. Several physical mechanisms were operative during the different stages of the storms. Fil: Mansilla, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina |
format |
Article in Journal/Newspaper |
author |
Mansilla, Gustavo Adolfo |
author_facet |
Mansilla, Gustavo Adolfo |
author_sort |
Mansilla, Gustavo Adolfo |
title |
Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
title_short |
Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
title_full |
Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
title_fullStr |
Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
title_full_unstemmed |
Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms |
title_sort |
response of the antarctic ionosphere to some intense geomagnetic storms |
publisher |
Bentham Open |
url |
http://hdl.handle.net/11336/67044 |
long_lat |
ENVELOPE(-63.200,-63.200,-64.683,-64.683) ENVELOPE(-62.917,-62.917,-64.833,-64.833) ENVELOPE(-67.167,-67.167,-66.383,-66.383) |
geographic |
Antarctic The Antarctic Argentina Tucumán Gustavo Mansilla |
geographic_facet |
Antarctic The Antarctic Argentina Tucumán Gustavo Mansilla |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
info:eu-repo/semantics/altIdentifier/url/http://benthamopen.com/ABSTRACT/TOASCJ-11-16 info:eu-repo/semantics/altIdentifier/doi/10.2174/1874282301711010016 http://hdl.handle.net/11336/67044 Mansilla, Gustavo Adolfo; Response of the Antarctic Ionosphere to Some Intense Geomagnetic Storms; Bentham Open; The Open Atmospheric Science Journal; 11; 1; 5-2017; 16-28 1874-2823 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.2174/1874282301711010016 |
container_title |
The Open Atmospheric Science Journal |
container_volume |
11 |
container_issue |
1 |
container_start_page |
16 |
op_container_end_page |
28 |
_version_ |
1779309591501209600 |