Laboratory study of low-beta forces in arched, line-tied magnetic flux ropes

Myers, Clayton ; Yamada, Masaaki ; Ji, Hantao ; Yoo, Jongsoo ; Jara-Almonte, Jonathan ; Fox, William
Issue date: 2016
Rights:
Creative Commons Attribution 4.0 International (CC BY)
Cite as:
Myers, Clayton, Yamada, Masaaki, Ji, Hantao, Yoo, Jongsoo, Jara-Almonte, Jonathan, & Fox, William. (2016). Laboratory study of low-beta forces in arched, line-tied magnetic flux ropes [Data set]. Princeton Plasma Physics Laboratory, Princeton University. https://doi.org/10.11578/1367081
@electronic{myers_clayton_2016,
  author      = {Myers, Clayton and
                Yamada, Masaaki and
                Ji, Hantao and
                Yoo, Jongsoo and
                Jara-Almonte, Jonathan and
                Fox, William},
  title       = {{Laboratory study of low-beta forces in a
                rched, line-tied magnetic flux ropes}},
  publisher   = {{Princeton Plasma Physics Laboratory, Pri
                nceton University}},
  year        = 2016,
  url         = {https://doi.org/10.11578/1367081}
}
Description:

The loss-of-equilibrium is a solar eruption mechanism whereby a sudden breakdown of the magnetohydrodynamic force balance in the Sun's corona ejects a massive burst of particles and energy into the heliosphere. Predicting a loss-of-equilibrium, which has more recently been formulated as the torus instability, relies on a detailed understanding of the various forces that hold the pre-eruption magnetic flux rope in equilibrium. Traditionally, idealized analytical force expressions are used to derive simplified eruption criteria that can be compared to solar observations and modeling. What is missing, however, is a validation that these idealized analytical force expressions can be applied to the line-tied, low-aspect-ratio conditions of the corona. In this paper, we address this shortcoming by using a laboratory experiment to study the forces that act on long-lived, arched, line-tied magnetic flux ropes. Three key force terms are evaluated over a wide range of experimental conditions: (1) the upward hoop force; (2) the downward strapping force; and (3) the downward toroidal field tension force. First, the laboratory force measurements show that, on average, the three aforementioned force terms cancel to produce a balanced line-tied equilibrium. This finding validates the laboratory force measurement techniques developed here, which were recently used to identify a dynamic toroidal field tension force that can prevent flux rope eruptions [Myers et al., Nature 528, 526 (2015)]. The verification of magnetic force balance also confirms the low-beta assumption that the plasma thermal pressure is negligible in these experiments. Next, the measured force terms are directly compared to their corresponding analytical expressions. While the measured and analytical forces are found to be well correlated, the low-aspect-ratio, line-tied conditions in the experiment are found to both reduce the measured hoop force and increase the measured tension force with respect to analytical expectations. These two co-directed effects combine to generate laboratory flux rope equilibria at lower altitudes than are predicted analytically. Such considerations are expected to modify the loss-of-equilibrium eruption criteria for analogous flux ropes in the solar corona.

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