Measurements of the polytropic index γ inside a magnetic cloud showed that there are two non-equal tubes inside the cloud [Fainberg et al., 1996; Osherovich et al., 1997]. For both tubes, γ < 1, but each tube has its own polytrope. We test equilibrium solutions which are a superposition of solutions with cylindrical and helical symmetry [Krat and Osherovich, 1978] as a new paradigm for a multi-tube model. Comparison of magnetic and gas pressure profiles for these bounded MHD states with observations suggests that complex magnetic clouds can be viewed as multiple helices embedded in a cylindrically symmetric flux rope.
CITATION STYLE
Osherovich, V. A., Fainberg, J., & Stone, R. G. (1999). Multi-tube model for interplanetary magnetic clouds. Geophysical Research Letters, 26(3), 401–404. https://doi.org/10.1029/1998GL900306
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