@article{ref1,
title="The current generated by deep water regular waves",
journal="Coastal engineering (Amsterdam)",
year="2017",
author="Bratland, A. K.",
volume="121",
number="",
pages="103-106",
abstract="Second-order mean drift of wave particles can in deep water be calculated using potential theory, resulting in the well-known Stokes drift. Potential theory assumes an ideal, incompressible and irrotational flow, which according to Longuet-Higgins [8] is not permanent. In this document it is recommended, for rotational flow, to add a current term to Stokes wave equations. This is based on the argument that a change in wave number is due to the onset of a current.<p /> <p>Language: en</p>",
language="en",
issn="0378-3839",
doi="10.1016/j.coastaleng.2016.12.003",
url="http://dx.doi.org/10.1016/j.coastaleng.2016.12.003"
}