Abstract

We consider the periodic Benjamin–Ono equation, regularized in the same way as the Benjamin–Bona–Mahony equation is found from the Korteweg–de Vries one [T.B. Benjamin, J.L. Bona, J.J. Mahony, Model equations for long waves in nonlinear dispersive systems, Philos. Trans. Roy. Soc. London Ser. A 272 (1220) (1972) 47–78], namely the equation u t + u x + α u u x + β H ( u x t ) = 0 , where H is the Hilbert transform, α the quotient between the characteristic wave amplitude and the depth of the waves and β the quotient between this depth and the wavelength. We show that the solution, starting from an initial datum of size ε , remains smaller than ε for a time scale of order ( ε − 1 β / α ) 2 , whereas the local well-posedness gives only a time of order ε − 1 β / α .

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