dor_id: 4141310

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590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1687/1840

100.1.#.a: G. De Alvarez, M.

524.#.#.a: G. De Alvarez, M. (1963). Definitions of the geomagnetic equator. Geofísica Internacional; Vol. 3 Núm. 2: Abril 1, 1963; 43-48. Recuperado de https://repositorio.unam.mx/contenidos/4141310

245.1.0.a: Definitions of the geomagnetic equator

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1963

264.#.1.c: 1964-04-01

653.#.#.a: Ecuador geomagnético; Curva de inclinación mínima; Radiación cósmica; Geomagnetic equator; Curve of minimum inclination; Cosmic radiation

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1687

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1687

041.#.7.h: spa

520.3.#.a: Different models of equators are exposed and the advantages of the equator defined by a normal plane to the dipole located in the magnetic terrestrial centre C are shown. The geomagnetic equator has a great interest in a number of geophysical problems. Magnetic charts with isoclinal curves are constructed with data obtained from observations of terrestrial magnetism. The real magnetic equator will he defined by the curve of minimum inclination, which is very irregular to be mathematically determined and considered in the physical models for other studies. In particular, the physicists doingwork on cosmic rays on which the magnetic field exerts an influence, have considered that the geomagnetic equator should be determined by minimal radiation points. Not only the curve would also be irregular, but these is also the inconvenience of lack of data for its study. When this paper was presented in the Mathematical Congress of the Mexican Mathematical Society, in the city of Merida, in September of 1960, there was unawareness of any publication on the empirical curve of cosmic radiation. In 1961, at the Postdam Geomagnetic Institute a graph was prepared in which that the cosmic ray equator, approximates the minimum inclination equator: Z = 0 (Fig. 1).

773.1.#.t: Geofísica Internacional; Vol. 3 Núm. 2: Abril 1, 1963; 43-48

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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300.#.#.a: Páginas: 43-48

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.2954436xe.1963.3.2.1687

handle: 66ab8a41c587bae0

harvesting_date: 2023-06-20 17:00:00.0

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file_modification_date: 2023-04-25 20:51:14.0

file_creator: M. G. de Alvarez

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245.1.0.b: Definiciones del Ecuador geomagnético

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license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Definitions of the geomagnetic equator

G. De Alvarez, M.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

G. De Alvarez, M. (1963). Definitions of the geomagnetic equator. Geofísica Internacional; Vol. 3 Núm. 2: Abril 1, 1963; 43-48. Recuperado de https://repositorio.unam.mx/contenidos/4141310

Descripción del recurso

Autor(es)
G. De Alvarez, M.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Definitions of the geomagnetic equator
Fecha
1964-04-01
Resumen
Different models of equators are exposed and the advantages of the equator defined by a normal plane to the dipole located in the magnetic terrestrial centre C are shown. The geomagnetic equator has a great interest in a number of geophysical problems. Magnetic charts with isoclinal curves are constructed with data obtained from observations of terrestrial magnetism. The real magnetic equator will he defined by the curve of minimum inclination, which is very irregular to be mathematically determined and considered in the physical models for other studies. In particular, the physicists doingwork on cosmic rays on which the magnetic field exerts an influence, have considered that the geomagnetic equator should be determined by minimal radiation points. Not only the curve would also be irregular, but these is also the inconvenience of lack of data for its study. When this paper was presented in the Mathematical Congress of the Mexican Mathematical Society, in the city of Merida, in September of 1960, there was unawareness of any publication on the empirical curve of cosmic radiation. In 1961, at the Postdam Geomagnetic Institute a graph was prepared in which that the cosmic ray equator, approximates the minimum inclination equator: Z = 0 (Fig. 1).
Tema
Ecuador geomagnético; Curva de inclinación mínima; Radiación cósmica; Geomagnetic equator; Curve of minimum inclination; Cosmic radiation
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces