Instability of current sheets and formation of plasmoid chains
TL;DR
Imagine you have two rubber bands stretched in opposite directions, and suddenly they snap back together. In space, magnetic field lines can do something similar - they can break apart and reconnect in explosive events. Scientists thought this happened in one smooth process, but this research shows it's actually much messier. Instead of one clean reconnection, the magnetic field lines become unstable and form a chain of smaller "bubbles" or islands (called plasmoids) that look like beads on a string. This happens much faster than scientists previously thought, and the number of these bubbles depends on how strong the magnetic field is. It's like instead of two rubber bands snapping together once, they create a whole chain of smaller snaps that happen very quickly.
Current sheets formed in magnetic reconnection events are found to be unstable to high-wavenumber perturbations. The instability is very fast: its maximum growth rate scales as S^{1/4} v_A/L, where L is the length of the sheet, v_A the Alfven speed and S the Lundquist number. As a result, a chain of plasmoids (secondary islands) is formed, whose number scales as S^{3/8}.
- 1Current sheets in magnetic reconnection events are unstable to high-wavenumber perturbations
- 2The instability growth rate scales as S^{1/4} v_A/L where S is the Lundquist number, v_A is the Alfven speed, and L is the sheet length
- 3The instability leads to formation of plasmoid chains (secondary islands)
- 4The number of plasmoids in the chain scales as S^{3/8}
- 5The instability is very fast compared to traditional reconnection timescales
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