The Gauss series is a widely used expression for the scalar magnetic potential of the Earth’s magnetic field . Recorded in geocentric spherical coordinates , , , it is used as an international standard for a normal geomagnetic field [1] :
Where:
- - distance from the center of the earth,
- - complement geographic latitude , that is, the polar angle,
- - longitude
- - standard radius of the Earth (6371.2 km),
- and - Gaussian coefficients, depending on time t [2] ,
- - Schmidt - normalized adjoint Legendre functions of degree n , of order m .
Literature
- IAGA Division V, Working group 8. International Geomagnetic Reference Field - Epoch 2005 Revision Of The IGRF for 2005-2010. (International Geomagnetic Field Standard - IGRF Review of the 2005 Era for 2005—2010)
- Volokhov S. A. et al. Spatial harmonic analysis of the magnetic field of technical objects by the method of integral transformations of magnetic signatures / S. A. Volokhov, A. V. Kildishev, P. N. Dobrodeev, L. F. Ivleva // Vestnik KhGPU, graduation 84, series НРСТ (New solutions in modern technologies). - Kharkov: KHGPU, 2000, C41-44.
Links
Notes
- ↑ IAGA V-MOD Geomagnetic Field Modeling: International Geomagnetic Reference Field IGRF-11
- ↑ Links to the coefficient table of the international standard for the era of 2005-2010 (IGRF-10) and the program for calculating the elements of the geomagnetic field are on the International Geomagnetic Reference Field page.