Since the magnetosheath plasma is highly turbulent, reconnection at the dayside magnetopause is likely to be temporally unsteady. The tearing mode can be viewed as a model for the unsteady development of a reconnecting magnetic topology. Magnetopause tearing occurs in the guide‐field limit and has a wave packet spatial structure in the east‐west direction. We solve for the nonlinear evolution of a single wavelength guide‐field tearing mode including the effects of finite transit time on the Landau resonant electrons. Short wavelength modes evolve algebraically in time with perturbation amplitudes proportional to t². Long wavelength modes are fully nonlinear, and the amplitude grows linearly in time.
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Coroniti et al. (1984) studied this question.
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