2013
DOI: 10.1007/s13131-013-0285-5
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Effect of Langmuir circulation on upper ocean mixing in the South China Sea

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Cited by 12 publications
(10 citation statements)
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“…When the wave spectrum is unavailable, the surface Stokes drift is usually estimated from the wind speed or wind stress using formulations such as, Us0=0.016|U10| [ Li and Garrett , ] and Us0=0.377|τ|1/2 [ Madec , ], where U 10 is the wind speed at 10 m above the sea surface level. Normally, the vertical profile of the Stokes drift is calculated assuming that the surface Stokes drift exponentially decrease with depth [ Polton et al ., ; Li et al ., ]. Breivik et al .…”
Section: Resultsmentioning
confidence: 96%
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“…When the wave spectrum is unavailable, the surface Stokes drift is usually estimated from the wind speed or wind stress using formulations such as, Us0=0.016|U10| [ Li and Garrett , ] and Us0=0.377|τ|1/2 [ Madec , ], where U 10 is the wind speed at 10 m above the sea surface level. Normally, the vertical profile of the Stokes drift is calculated assuming that the surface Stokes drift exponentially decrease with depth [ Polton et al ., ; Li et al ., ]. Breivik et al .…”
Section: Resultsmentioning
confidence: 96%
“…Breivik et al . [] proposed a new method for estimating this vertical profile, which they demonstrate considerably improves the exponentially decreasing method [ Polton et al ., ; Li et al ., ], as follows: boldus(z)=boldus0e2kez18kez where k e is the inverse depth scale; for details see Breivik et al . [].…”
Section: Resultsmentioning
confidence: 96%
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