作者: A. Egidi , D. Del Moro , F. Berrilli , B. Viticchié
DOI:
关键词: Dipole model of the Earth's magnetic field 、 Computational physics 、 Magnetic energy 、 Geophysics 、 Magnetic field 、 Distribution function 、 L-shell 、 Magnetic reconnection 、 Vector field 、 Advection 、 Physics
摘要: We present a dynamic model of atmospheric magnetic field in which loop footpoints are advected by velocity computed using simple n-body simula- tion and reproducing large spatial organization scales (e.g. mesogranulation). In this model, the advection passive elements triggers multiple reconnection processes forc- ing reconfigurations ensuing fluctuations total energy. The simulations reproduce system with scale-free properties, provides frequency distribution functions for emitted energies, described power-law index 2:4, also quiescent times between di erent energy emissions.