2022
DOI: 10.1029/2022jc018941
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Relating a Large‐Scale Variation of Waves in the Indian Ocean to the IOD

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 6 publications
(6 citation statements)
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“…Compared to wind seas, swells are smoother and have faster propagation speeds and longer wavelengths (and periods). What is more, swells can travel long distances and transfer energy across the entire ocean [1][2][3], and they typically have a dominant energy contribution, as demonstrated by both Semedo et al and Chen et al [4,5]. Although swells seem to be gentle, they can also pose a threat to shipping activities.…”
Section: Introductionmentioning
confidence: 99%
“…Compared to wind seas, swells are smoother and have faster propagation speeds and longer wavelengths (and periods). What is more, swells can travel long distances and transfer energy across the entire ocean [1][2][3], and they typically have a dominant energy contribution, as demonstrated by both Semedo et al and Chen et al [4,5]. Although swells seem to be gentle, they can also pose a threat to shipping activities.…”
Section: Introductionmentioning
confidence: 99%
“…The main focus of this paper is on the effects of meridional wave transport. In our study of the relationship between IOD and wave transport in the Indian Ocean [43], we concentrate on zonal transport. Zonal wave transport can also significantly impact the IOD.…”
Section: Discussionmentioning
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%