Solar quiet geomagnetic variations and E-region neutral winds at equatorial latitudes

A model of the ionospheric current system valid at zones close to the geomagnetic equator, taking into account the contribution of neutral winds, is proposed. From this, the external magnetic field at ground is calculated. Also, ground records of the geomagnetic field variations at the Peruvian equa...

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Autor principal: de la Vega, M.
Otros Autores: Favetto, Alicia Beatriz, Osella, Ana María
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 1995
Acceso en línea:Registro en Scopus
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Registro en la Biblioteca Digital
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245 1 0 |a Solar quiet geomagnetic variations and E-region neutral winds at equatorial latitudes 
260 |c 1995 
270 1 0 |m de la Vega, M.; Dto. Fisica -Fac. Cs. Exactas, Naturales Universidad de Buenos Aires Ciudad Universitaria - Pab, I 1428 Buenos Aires, Argentina 
504 |a Anderson, Forbes, Codrescu, A fully analytic, low- and middle-latitude ionospheric model (1989) Journal of Geophysical Research, 94, p. 1520 
504 |a Banks, (1966) Planet Space Sci., 14, p. 1085 
504 |a Banks, (1966) Planet Space Sci., 14, p. 1105 
504 |a Bedinger, (1977) J. atmos. terr. Phys., 39, p. 241 
504 |a Berdichevsky, Zhdanov, (1984) Advanced theory of deep geomagnetic sounding, , Elsevier 
504 |a Burrows, The day-to-day variability of the equatorial electrojet in Peru (1970) Journal of Geophysical Research, 75, p. 1319 
504 |a Chapman, The electrical conductivity of the ionosphere: A review (1956) Il Nuovo Cimento, 10, p. 1385 
504 |a Duhau, Azpiazu, (1985) Planet. Space Sci., 33, p. 909 
504 |a Forbes, Atmospheric tides: 1. Model description and results for the solar diurnal component (1982) Journal of Geophysical Research, 87, p. 5222 
504 |a Forbes, Atmospheric tide: 2. The solar and lunar semidiurnal components (1982) Journal of Geophysical Research, 87, p. 5241 
504 |a Forbes, Lindzen, (1976) J. atmos. terr. Phys., 38, p. 911 
504 |a Forbush and Casaverde 1961 Carnegie Inst. Wash. Publ. 620pp; Onwumechili, Study of the Return Current of the Equatorial Electrojet. (1992) Journal of geomagnetism and geoelectricity, 44, p. 1 
504 |a Osella, Favetto, Martinelli, (1993) Trends in Geophs. Res., 2, p. 141 
504 |a Richmond, (1973) J. atmos. terr. Phys., 35, p. 1083 
504 |a Stening, (1969) Planet. Space Sci., 18, p. 1091 
504 |a Stening, A calculation of ionospheric currents due to semidiurnal antisymmetric tides (1989) Journal of Geophysical Research, 94, p. 1525 
504 |a Takeda, Maeda, Three-dimensional structure of ionospheric currents 1. Currents caused by diurnal tidal winds (1980) Journal of Geophysical Research, 85, p. 6895 
504 |a Tarpley, (1970) Planet. Space Sci., 18, p. 1091 
504 |a Woodman, Vertical drift velocities and east-west electric fields at the magnetic equator (1970) Journal of Geophysical Research, 75, p. 6249 
506 |2 openaire  |e Política editorial 
520 3 |a A model of the ionospheric current system valid at zones close to the geomagnetic equator, taking into account the contribution of neutral winds, is proposed. From this, the external magnetic field at ground is calculated. Also, ground records of the geomagnetic field variations at the Peruvian equatorial zone were separated into their external and internal contributions. Using an iterative process a local particular fitting was found by comparing the separated external field to the one calculated with the proposed model. © 1995.  |l eng 
593 |a Dto. Fisica -Fac. Cs. Exactas, Naturales Universidad de Buenos Aires Ciudad Universitaria - Pab, I 1428 Buenos Aires, Argentina 
700 1 |a Favetto, Alicia Beatriz 
700 1 |a Osella, Ana María 
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