http://dx.doi.org/10.4153/CMB-2011-057-3
Canad. Math. Bull. 55(2012), 176-187
Published:2011-03-31 Printed: Mar 2012
Daniel Spirn, School of Mathematics, University of Minnesota, Minneapolis, MN 55455, U.S.A.
J. Douglas Wright, Department of Mathematics, Drexel University, Philadelphia, PA 19104, U.S.A.
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Abstract
We consider the linearization of the three-dimensional water waves
equation with surface tension about a flat interface. Using
oscillatory integral methods, we prove that solutions of this equation
demonstrate dispersive decay at the somewhat surprising rate of
$t^{-5/6}$. This rate is due to competition between surface tension
and gravitation at $O(1)$ wave numbers and is connected to the fact
that, in the presence of surface tension, there is a so-called "slowest
wave". Additionally, we combine our dispersive estimates with $L^2$
type energy bounds to prove a family of Strichartz estimates.
© Canadian Mathematical Society, 2013
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