CONDITIONS FOR PHOTOSPHERICALLY DRIVEN ALFVENIC OSCILLATIONS TO HEAT THE SOLAR CHROMOSPHERE BY PEDERSEN CURRENT DISSIPATION

Amagnetohydrodynamic 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 observed net chromospheric radiative loss of similar to 10(7) erg cm(-2) s(-1). 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 F-Ch similar to 10(7)-10(8) erg cm(-2) s(-1) at frequencies nu similar to 10(2)-10(3) mHz for BG magnetic field strengths B greater than or similar to 700 G and magnetic field perturbation amplitudes similar to 0.01-0.1 B. 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 FCh. FCh 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 similar to 10 m in the photosphere to similar to 10 km in the upper chromosphere and is proportional to nu(-1/2). Estimates suggest that these oscillations are normal modes of photospheric flux tubes with diameters similar to 10-20 km, excited by magnetic reconnection in current sheets with thicknesses similar to 0.1 km.