Indication of anomalous conductivity at the nigerian dip equator

The geomagnetic daily variations at the Nigerian dip equator have been analyzed with the methodology introduced in a previous paper. It has been found that the height integrated current presents a notoriously higher amplification in Nigeria than in Peru. It has also been found that there exists a st...

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Detalles Bibliográficos
Autor principal: Duhau, Silvia Noemí Catalina
Otros Autores: Romanelli, Lilia Mabel, Hirsch, F.A
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 1982
Acceso en línea:Registro en Scopus
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Registro en la Biblioteca Digital
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100 1 |a Duhau, Silvia Noemí Catalina 
245 1 0 |a Indication of anomalous conductivity at the nigerian dip equator 
260 |c 1982 
270 1 0 |m Duhau, S.; Departamento de Física, Facultad de Ciencias Exactas y Naturales (UBA), Buenos Aires, Argentina 
504 |a Duhau, Romanelli, Correction [to “Five structure instabilities induced by double diffusion in the shelf/slope water front”] (1979) Journal of Geophysical Research, 84, p. 1847 
504 |a Duhau, Romanelli, (1981) Planet. Space Sci., 29, p. 703 
504 |a Romanelli, Hirsch, Duhau, (1981) Geoacta, 11. , (in press) 
504 |a Gagnepain, Crochet, Richmond, (1977) J. atmos. terr. Phys., 39, p. 1119 
504 |a Ogbuehi, Onwumechilli, (1964) J. atmos. terr. Phys., 26, p. 889 
504 |a Onwumechilli, (1967) Physics Geomagnetic Phenomena, 1, p. 427. , Academic Press, New York 
504 |a Richmond, (1973) J. atmos. terr. Phys., 35, p. 1105 
504 |a Untiedt, A model of the equatorial electrojet involving meridional currents (1967) Journal of Geophysical Research, 72, p. 5799 
506 |2 openaire  |e Política editorial 
520 3 |a The geomagnetic daily variations at the Nigerian dip equator have been analyzed with the methodology introduced in a previous paper. It has been found that the height integrated current presents a notoriously higher amplification in Nigeria than in Peru. It has also been found that there exists a strong and inhomogeneous anomaly in the Earth's conductivity in Nigeria. And contrary to what is usually accepted, it is shown that its latitudinal distribution can not be precisely determined until the distribution and magnitude of the ionospheric currents at F-region heights is more accurately known. © 1982.  |l eng 
593 |a Departamento de Física, Facultad de Ciencias Exactas y Naturales (UBA), Buenos Aires, Argentina 
700 1 |a Romanelli, Lilia Mabel 
700 1 |a Hirsch, F.A. 
773 0 |d 1982  |g v. 30  |h pp. 97-100  |k n. 1  |p Planet. Space Sci.  |x 00320633  |w (AR-BaUEN)CENRE-2228  |t Planetary and Space Science 
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