We study the nonlinear evolution of the resistive tearing mode in slab geometry in two dimensions. We show that, in the strongly driven regime (large Δ^'), a collapse of the X point occurs once the island width exceeds a certain critical value ~1/Δ^'. A current sheet is formed and the reconnection is exponential in time with a growth rate ∝η1/2, where η is the resistivity. If the aspect ratio of the current sheet is sufficiently large, the sheet can itself become tearing-mode unstable, giving rise to secondary islands, which then coalesce with the original island. The saturated state depends on the value of Δ^'. For small Δ^', the saturation amplitude is ∝Δ^' and quantitatively agrees with the theoretical prediction. If Δ^' is large enough for the X-point collapse to have occurred, the saturation amplitude increases noticeably and becomes independent of Δ^'.
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Loureiro et al. (2005) studied this question.
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