Let . The nonlinear term has two perpendicular spatial derivatives, so its rate relative to the fluctuation amplitude is
The wave period from part (a), using , is . A weak wave cascade requires that one interaction change a packet only slightly:
For interactions with decorrelated phases, successive fractional changes accumulate as a random walk. An order-one change needs , giving
Constant energy flux per unit mass then gives , hence
The weak electron-magnetohydrodynamic cascade scaling uses both locality in scale and the decorrelation assumption; a small amplitude by itself does not specify the cascade time.

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