The treatment of Alfvén wave mode decay by Cohen and Dewar (1974) is extended to a regime of finite temperature and large acoustic wave damping rates for a model (Lorentzian) Alfvén wave power spectrum. When applied to hydromagnetic waves in the solar wind, the theory predicts a degradation of the low-frequency (∼(1 day)−1) portion of the spectrum on a time scale of the order of the time required for such waves to travel several AU.
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Ronald H. Cohen (1975) studied this question.
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