Stokes drift and its discontents

Jacques Vanneste, William R. Young

Research output: Contribution to journalArticlepeer-review

Abstract

The Stokes velocity uS, defined approximately by Stokes (1847, Trans. Camb. Philos. Soc., 8, 441–455), and exactly via the Generalized Lagrangian Mean,
is divergent even in an incompressible fluid. We show that the Stokes velocity can be naturally decomposed into a solenoidal component, uS sol, and
a remainder that is small for waves with slowly varying amplitudes. We further show that uS sol arises as the sole Stokes velocity when the Lagrangian
mean flow is suitably redefined to ensure its exact incompressibility. The construction is an application of Soward & Roberts’s glmtheory (2010, J. FluidMech., 661, 45–72) which we specialise to surface gravity
waves and implement effectively using a Lie series expansion. We further show that the corresponding Lagrangian-mean momentum equation is formally
identical to the Craik–Leibovich equation with uS sol replacing uS, and we discuss the form of the Stokes pumping associated with both uS and uS
sol.
Original languageEnglish
Article number20210032
Number of pages15
JournalPhilosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Volume380
Issue number2225
Early online date25 Apr 2022
DOIs
Publication statusPublished - 13 Jun 2022

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