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Solar-wind properties at the Earth as predicted by the two-fluid model

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Abstract

The two-fluid equations for the solar wind are written down in a simplified form, similar to that suggested by Roberts (1971) for the one-fluid model. The equations are shown to depend only on one parameter,

$$K = GM\kappa _e m_p (\varepsilon _\infty T_0 )^{{3 \mathord{\left/ {\vphantom {3 2}} \right. \kern-\nulldelimiterspace} 2}} /4k^2 Fe,$$

, where G is the gravitational constant, M the mass of the star, κ e the thermal electron conductivity, m p the proton mass, k the Boltzman constant, T0 the residual energy per particle at infinity and F e the electron-particle flux. For a variety of values of the density and temperature at the base of the corona we compute the solutions of the two-fluid solar wind model and compare the predicted and observed solar wind parameters at the Earth.

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The National Center for Atmospheric Research is sponsored by the National Science Foundation.

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Durney, B.R. Solar-wind properties at the Earth as predicted by the two-fluid model. Sol Phys 30, 223–234 (1973). https://doi.org/10.1007/BF00156191

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  • DOI: https://doi.org/10.1007/BF00156191

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