Third-order theory and numerical trajectory integration show classical Stokes drift underestimates surface particle drift and overestimates it at depth; adding difference harmonics improves agreement for regular and irregular waves.
& Vertenstein, M 2016 Langmuir mixing effects on global climate: Wavewatch iii in cesm
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Wave-induced drift in third-order deep-water theory
Third-order theory and numerical trajectory integration show classical Stokes drift underestimates surface particle drift and overestimates it at depth; adding difference harmonics improves agreement for regular and irregular waves.