Gaussian method for computing the Earth’s magnetic field

Doneva, Blagica (2020) Gaussian method for computing the Earth’s magnetic field. Balkan Journal of Applied Mathematics and Informatics (BJAMI), 3 (1). pp. 95-106. ISSN 2545-4803

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Abstract

For the study of the geomagnetic phenomena and the solving of numerous tasks from the application of geomagnetic methods, it is very important to find an analytical
expression that shows the dependence of the magnetic field, or of its components, on the coordinates of the points placed on the Earth's surface. To find such an analytic
expression, one can start from the assumption of a homogeneously magnetized Earth, or, based on the measured values of the elements of the Earth's magnetic field at a set point, an expression can be found that shows the distribution of magnetization inside the Earth
corresponding to the measured field. The elements of the geomagnetic field are: declination D, inclination I, horizontal H, eastern Y, northern X and vertical Z component, as well as the vector T of the geomagnetic field. The intensities of the geomagnetic field
elements are expressed in [nT] nanotesla, and the values of declination D and inclination I of the geomagnetic field are expressed in degrees.

Item Type: Article
Subjects: Natural sciences > Earth and related environmental sciences
Divisions: Faculty of Natural and Technical Sciences
Depositing User: Blagica Doneva
Date Deposited: 26 Jun 2020 07:27
Last Modified: 26 Jun 2020 07:27
URI: https://eprints.ugd.edu.mk/id/eprint/24142

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