Conditions for Photospherically Driven Alfvenic Oscillations to Heat the Solar Chromosphere by Pedersen Current Dissipation
arXiv:1410.8519 · doi:10.1088/0004-637X/735/1/45
Abstract
A magnetohydrodynamic model that includes a complete electrical conductivity tensor is used to estimate conditions for photospherically driven, linear, non-plane Alfvenic oscillations extending from the photosphere to the lower corona to drive a chromospheric heating rate due to Pedersen current dissipation that is comparable to the net chromospheric net radiative loss of ergs-cm-sec. The heating rates due to electron current dissipation in the photosphere and corona are also computed. The wave amplitudes are computed self-consistently as functions of an inhomogeneous background (BG) atmosphere. The effects of the conductivity tensor are resolved numerically using a resolution of 3.33 m. The oscillations drive a chromospheric heating flux ergs-cm-sec at frequencies mHz for BG magnetic field strengths G and magnetic field perturbation amplitudes . The total resistive heating flux increases with . Most heating occurs in the photosphere. Thermalization of Poynting flux in the photosphere due to electron current dissipation regulates the Poynting flux into the chromosphere, limiting . initially increases with , reaches a maximum, and then decreases with increasing due to increasing electron current dissipation in the photosphere. The resolution needed to resolve the oscillations increases from m in the photosphere to km in the upper chromosphere, and is proportional to . Estimates suggest that these oscillations are normal modes of photospheric flux tubes with diameters km, excited by magnetic reconnection in current sheets with thicknesses km.
55 pages, 19 figures
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