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Undid revision 671030225 by 71.184.20.127 (talk) restore figure: Stokes drift is one of the relevant factors in the transport of marine debris |
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*{{cite journal | author= M.S. Longuet-Higgins | authorlink=Michael S. Longuet-Higgins | year= 1953 | title= Mass transport in water waves | journal= Philosophical Transactions of the Royal Society A | volume= 245 | pages= 535–581 | url= http://rsta.royalsocietypublishing.org/content/245/903/535 | doi= 10.1098/rsta.1953.0006 |bibcode = 1953RSPTA.245..535L | issue=903|ref=Longuet-Higgins1953}}
*{{cite book| first=O.M. | last=Phillips | title=The dynamics of the upper ocean |publisher=Cambridge University Press | year=1977 | edition=2nd | isbn=0-521-29801-6 |ref=Phillips1977}}
*{{cite book | author=G. Falkovich| year=2011 | title=Fluid Mechanics (A short course for physicists)
*{{cite journal | title=A mechanism for the accumulation of floating marine debris North of Hawaii | last=Kubota |first=M. |year=1994 |doi=10.1175/1520-0485(1994)024<1059:AMFTAO>2.0.CO;2 |journal=Journal of Physical Oceanography |volume=24 |issue=5 |pages=1059–1064 |ref=Kubota1994 }}
==Notes==
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