Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes
- Autores
- Mansilla, Gustavo Adolfo
- Año de publicación
- 2011
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- This paper reports the global response of the mid high and low latitude ionosphere in four longitudinal sectors to two moderate geomagnetic storms that occurred during 2007 (the more intense storms occurred that year). The results obtained during these storms show that the ionospheric effects in general are not moderate in magnitude, showing an important degree of complexity as during intense storms. The outstanding features produced during the storms are significant positive storm effects at mid-high latitudes during the main phase/first part of the recovery, positive effects after the onset of the storm followed by negatives effects at middle latitudes and delayed positive effects during the night-time hours in the trough of the equatorial anomaly ("dusk" effect). Possible physical mechanisms for controlling the morphology of the ionosphere during these events are considered.
Fil: Mansilla, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina - Materia
-
Geomagnetic Storm
Ionosphere
Physical Mechanisms - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/72074
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Moderate geomagnetic storms and their ionospheric effects at middle and low latitudesMansilla, Gustavo AdolfoGeomagnetic StormIonospherePhysical Mechanismshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This paper reports the global response of the mid high and low latitude ionosphere in four longitudinal sectors to two moderate geomagnetic storms that occurred during 2007 (the more intense storms occurred that year). The results obtained during these storms show that the ionospheric effects in general are not moderate in magnitude, showing an important degree of complexity as during intense storms. The outstanding features produced during the storms are significant positive storm effects at mid-high latitudes during the main phase/first part of the recovery, positive effects after the onset of the storm followed by negatives effects at middle latitudes and delayed positive effects during the night-time hours in the trough of the equatorial anomaly ("dusk" effect). Possible physical mechanisms for controlling the morphology of the ionosphere during these events are considered.Fil: Mansilla, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; ArgentinaElsevier2011-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/72074Mansilla, Gustavo Adolfo; Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes; Elsevier; Advances in Space Research; 48; 3; 8-2011; 478-4870273-1177CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.asr.2011.03.034info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0273117711002158info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:09:51Zoai:ri.conicet.gov.ar:11336/72074instacron: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:34982025-09-10 13:09:51.519CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
title |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
spellingShingle |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes Mansilla, Gustavo Adolfo Geomagnetic Storm Ionosphere Physical Mechanisms |
title_short |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
title_full |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
title_fullStr |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
title_full_unstemmed |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
title_sort |
Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes |
dc.creator.none.fl_str_mv |
Mansilla, Gustavo Adolfo |
author |
Mansilla, Gustavo Adolfo |
author_facet |
Mansilla, Gustavo Adolfo |
author_role |
author |
dc.subject.none.fl_str_mv |
Geomagnetic Storm Ionosphere Physical Mechanisms |
topic |
Geomagnetic Storm Ionosphere Physical Mechanisms |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
This paper reports the global response of the mid high and low latitude ionosphere in four longitudinal sectors to two moderate geomagnetic storms that occurred during 2007 (the more intense storms occurred that year). The results obtained during these storms show that the ionospheric effects in general are not moderate in magnitude, showing an important degree of complexity as during intense storms. The outstanding features produced during the storms are significant positive storm effects at mid-high latitudes during the main phase/first part of the recovery, positive effects after the onset of the storm followed by negatives effects at middle latitudes and delayed positive effects during the night-time hours in the trough of the equatorial anomaly ("dusk" effect). Possible physical mechanisms for controlling the morphology of the ionosphere during these events are considered. Fil: Mansilla, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina |
description |
This paper reports the global response of the mid high and low latitude ionosphere in four longitudinal sectors to two moderate geomagnetic storms that occurred during 2007 (the more intense storms occurred that year). The results obtained during these storms show that the ionospheric effects in general are not moderate in magnitude, showing an important degree of complexity as during intense storms. The outstanding features produced during the storms are significant positive storm effects at mid-high latitudes during the main phase/first part of the recovery, positive effects after the onset of the storm followed by negatives effects at middle latitudes and delayed positive effects during the night-time hours in the trough of the equatorial anomaly ("dusk" effect). Possible physical mechanisms for controlling the morphology of the ionosphere during these events are considered. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-08 |
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/11336/72074 Mansilla, Gustavo Adolfo; Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes; Elsevier; Advances in Space Research; 48; 3; 8-2011; 478-487 0273-1177 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/72074 |
identifier_str_mv |
Mansilla, Gustavo Adolfo; Moderate geomagnetic storms and their ionospheric effects at middle and low latitudes; Elsevier; Advances in Space Research; 48; 3; 8-2011; 478-487 0273-1177 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.asr.2011.03.034 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0273117711002158 |
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 |
Elsevier |
publisher.none.fl_str_mv |
Elsevier |
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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1842980489217966080 |
score |
12.993085 |