2022
DOI: 10.1029/2022jc018941
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Abstract: Wind-generated ocean surface waves give rise to a near-surface velocity known as Stokes drift (SD) (Stokes, 1847), which can contribute substantially to near-surface mass transport. SD is widely applied in representation of nearshore circulation in coastal zones and in modeling of tracer transport as the difference between Lagrangian and Eulerian averages, and it is responsible for the Coriolis-Stokes force in the upper-ocean layer in Eulerian models (van den Bremer & Breivik, 2018). It has been shown that wav… Show more

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Cited by 5 publications
(1 citation statement)
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“…The impacts of concurrent events (e.g., ENSO + Southern Annular Mode [SAM]) on the wave or wind parameters can also be explored by using composites during positive/negative phases of the cooccurrence (Godoi & Torres Júnior, 2020; Ramos et al., 2021). The propagation of waves across oceanic basins could also interact with climate variability (Li et al., 2021, 2022; A. G. Marshall et al., 2018). Li et al.…”
Section: Introductionmentioning
confidence: 99%
“…The impacts of concurrent events (e.g., ENSO + Southern Annular Mode [SAM]) on the wave or wind parameters can also be explored by using composites during positive/negative phases of the cooccurrence (Godoi & Torres Júnior, 2020; Ramos et al., 2021). The propagation of waves across oceanic basins could also interact with climate variability (Li et al., 2021, 2022; A. G. Marshall et al., 2018). Li et al.…”
Section: Introductionmentioning
confidence: 99%