The Energy Lost by Differential Rotation in the Generation of the Solar Toroidal Magnetic Field

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Scientific paper

The integrals, I_i(t) = ∫_GL u_i j × B_idv over the volume GL are calculated in a dynamo model of the Babcock-Leighton type studied earlier. Here, GL is the generating layer for the solar toroidal magnetic field, located at the base of the solar convection zone (SCZ); i=r, θ, φ, stands for the radial, latitudinal, and azimuthal coordinates respectively; j = (4π)^-1∇ × B, where B is the magnetic field; u_r,u_θ are the components of the meridional motion, and u_φ is the differential rotation. During a ten-year cycle the energy ∫_cycle I_φ(t)dt needs to be supplied to the azimuthal flow in the GL to compensate for the energy losses due to the Lorentz force. The calculations proceed as follows: for every time step, the maximum value of |B_φ| in the GL is computed. If this value exceeds B_cr (a prescribed field) then there is eruption of a flux tube that rises radially, and reaches the surface at a latitude corresponding to the maximum of |B_φ| (the time of rise is neglected). This flux tube generates a bipolar magnetic region, which is replaced by its equivalent axisymmetric configuration, a magnetic ring doublet. The erupted flux can be multiplied by a factor F_t, i.e., by the number of eruptions per time step. The model is marginally stable and the ensemble of eruptions acts as the source for the poloidal field. The arbitrary parameters B_cr and F_t are determined by matching the flux of a typical solar active region, and of the total erupted flux in a cycle, respectively. If E(B) is the energy, in the GL, of the toroidal magnetic field B_φ = B sin θ cos θ, B (constant), then the numerical calculations show that the energy that needs to be supplied to the differential rotation during a ten-year cycle is of the order of E(B_cr), which is considerably smaller than the kinetic energy of differential rotation in the GL. Assuming that these results can be extrapolated to larger values of B_cr, magnetic fields ~10^4 G, could be generated in the upper section of the tachocline that lies below the SCZ (designated by UT). The energy required to generate these 10^4 G fields during a cycle is of the order of the kinetic energy in the UT.

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