A method for the interpretation of three-dimensional equatorial GDV fields

The equatorial GDV fields have been widely measured in North-South magnetometer chains and the data so obtained interpreted by assuming that these variations are bi-dimensional. This hypothesis limits its application to the inference of the noon amplitude of the ionospheric current and to the case o...

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Detalles Bibliográficos
Autores principales:	Duhau, S., Martínez, E.A.
Formato:	JOUR
Materias:	geomagnetic variation
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_13438832_v50_n2_p141_Duhau
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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