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dc.contributor.author
Cabrera, Miguel Angel  
dc.contributor.author
Ezquer, Rodolfo Gerardo  
dc.contributor.author
Spalla, Paolo  
dc.date.available
2019-09-27T13:56:33Z  
dc.date.issued
2006-12  
dc.identifier.citation
Cabrera, Miguel Angel; Ezquer, Rodolfo Gerardo; Spalla, Paolo; Slant total electron content for sirio-mortelliccio ray path; Editrice Compositori; Annals of Geophysics; 49; 4-5; 12-2006; 891-895  
dc.identifier.issn
1593-5213  
dc.identifier.uri
http://hdl.handle.net/11336/84648  
dc.description.abstract
The Total Electron Content (TEC) is used to indicate the ionisation of the ionosphere. TEC is a quantity that concern for predicting space weather effects on telecommunications, improving the accuracy of satellite navigation, fly control vehicles and other systems that use transionospheric signals, because the ionospheric layer affects the mentioned signals. In this work the Slant Total Electron Content (STEC) was calculated with a technique that uses so-called «auxiliaries stations model», and a Chapman layer with scale height equal to atomic oxygen scale height (CHO). The validity was checked with STEC measurements obtained from geosynchronous satellite signals, for SIRIO-Mortelliccio link considering solstices and equinox, in high solar activity period. In general, the deviations between predictions and measurements were lower than 30% for 16 h per day (average). The results suggest that additional studies for other links and solar activity are required in order to improve the model predictions.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Editrice Compositori  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Total Electron Content  
dc.subject
Ionosphere  
dc.subject
Space Weather  
dc.subject
Satellite  
dc.subject.classification
Geoquímica y Geofísica  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Slant total electron content for sirio-mortelliccio ray path  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2019-09-13T14:03:45Z  
dc.journal.volume
49  
dc.journal.number
4-5  
dc.journal.pagination
891-895  
dc.journal.pais
Italia  
dc.journal.ciudad
Bologna  
dc.description.fil
Fil: Cabrera, Miguel Angel. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física. Laboratorio de Ionósfera; Argentina  
dc.description.fil
Fil: Ezquer, Rodolfo Gerardo. Universidad Tecnológica Nacional. Facultad Regional Tucuman; Argentina. 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. Laboratorio de Ionósfera; Argentina  
dc.description.fil
Fil: Spalla, Paolo. Universidad Tecnológica Nacional. Facultad Regional Tucuman; Argentina  
dc.journal.title
Annals of Geophysics  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://dx.doi.org/10.4401/ag-3105  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.annalsofgeophysics.eu/index.php/annals/article/view/3105/3150