By R. S. Johnson

For over 100 years, the speculation of water waves has been a resource of exciting and sometimes tricky mathematical difficulties. almost each classical mathematical procedure looks someplace inside its confines. starting with the advent of the precise equations of fluid mechanics, the outlet chapters of this article ponder the classical difficulties in linear and nonlinear water-wave idea. This units the degree for a learn of extra sleek elements, difficulties that provide upward push to soliton-type equations. The e-book closes with an advent to the consequences of viscosity. the entire mathematical advancements are offered within the simplest demeanour, with labored examples and easy circumstances conscientiously defined. workouts, additional studying, and ancient notes on many of the very important characters within the box around off the ebook and make this an excellent textual content for a starting graduate path on water waves.

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**Extra info for A Modern Introduction to the Mathematical Theory of Water Waves**

**Sample text**

B) Now obtain the acceleration of the particle from the Lagrangian description. (c) Also write down the Eulerian acceleration, du/dt, where u = u(x, t). 7 where u = u(x, 0 Incompressible flows. 6 (a) all satisfy the condition for an incompressible flow, namely V • u = 0.

86). In practice, asymptotic expansions are rarely taken beyond a few terms, but it must be possible - in principle - to find them all. This representation is merely a compact way of describing a sequence of limiting processes (as x -> x0) on the functions \f(x)/go(x)}, [{f(x) ~ go(x)}/g\(•*)]> etc - However, the functions that we shall be working with involve one (or more) parameters; this is now introduced into our definition. The elements of wave propagation and asymptotic expansions 37 The asymptotic expansions that we require are defined with respect to a parameter, s say, as e -> 0, at fixed x.

98), will also be non-uniform at any values of £ for which the first, second, or third derivatives o f / © are undefined; we do not normally countenance this possibility in these types of problem. 99)) is usually called the far-field; the corresponding region for t = O(l) is then referred to as the near-field. 7. 94), makes use of the identities d _ d Yx = ^ 9 _ a and Jt = 3 8 Yx'Jr then the equation for u{x, t; s) = U{%, r; s) becomes sUrT - 2UTH = (U2 + Un)s. 7. A schematic representation of the far-field, where x = O(e l), t = O(s~l), with x-t = O(l); the wavefront is x- t = 0.