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Stokes drift and its discontents
Jacques Vanneste1, William R Young2
1School of Mathematics and Maxwell Institute for Mathematical Sciences, University of Edinburgh, Edinburgh EH9 3FD, UK.
Summary
We show that the divergent Stokes velocity can be decomposed into a solenoidal part and a small remainder for surface gravity waves. Redefining the Lagrangian mean flow yields an incompressible mean, resulting in a purely solenoidal Stokes velocity.
Area of Science:
- Fluid dynamics
- Wave theory
- Mathematical physics
Background:
- The Stokes velocity, fundamental in fluid dynamics, is known to be divergent even in incompressible fluids.
- Existing definitions, while useful, present challenges in fully describing fluid motion under wave influence.
Purpose of the Study:
- To decompose the divergent Stokes velocity into physically meaningful components.
- To develop an incompressible Lagrangian mean flow for accurate wave dynamics.
- To explore the implications for momentum equations and Stokes pumping.
Main Methods:
- Application of Generalized Lagrangian Mean (GLM) theory specialized for surface gravity waves.
- Utilizing Lie series expansion for effective implementation.
- Decomposition of Stokes velocity into solenoidal and remainder components.
Main Results:
- The Stokes velocity is shown to be decomposable into a solenoidal component and a remainder term.
- A redefined, exactly incompressible Lagrangian mean flow leads to a purely solenoidal Stokes velocity.
- The derived Lagrangian-mean momentum equation is analogous to the Craik-Leibovich equation.
Conclusions:
- The decomposition offers a more refined understanding of wave-induced fluid transport.
- The construction provides a novel approach to handling wave dynamics in fluid mechanics.
- This work contributes to the mathematical understanding of physical fluid dynamics.
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