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dc.contributor.authorRobin Robertson
dc.contributor.authorChangming Dong
dc.date.accessioned2020-10-10T02:37:17Z
dc.date.available2020-10-10T02:37:17Z
dc.date.issued2019-12-10
dc.identifier.citationGeoscience Letters,2019,(1)
dc.identifier.other10.1186/s40562-019-0146-y
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/175003
dc.description.abstractAbstract(#br)Vertical mixing is important in the ocean for maintaining its stratification, redistributing temperature and salinity, distributing nutrients and pollutants, and the energy cascade. It plays a key role in ocean energy transport, climate change, and marine ecosystems. Getting the mixing right in ocean circulation and climate models is critical in reproducing ocean and climate physics. Ocean models, like the Regional Ocean Modeling System (Rutgers ROMS 3.4), provide several options for determining vertical mixing through the vertical mixing parameterization schemes. To evaluate which of these methods best reproduces realistic vertical mixing by internal tides, simulations of baroclinic tides generated by a seamount were performed using seven different vertical mixing...
dc.language.isozh_CN
dc.subjectVertical mixing
dc.subjectMixing parameterizations
dc.subjectTides
dc.subjectSigma-coordinate models
dc.subjectSeamount
dc.titleAn evaluation of the performance of vertical mixing parameterizations for tidal mixing in the Regional Ocean Modeling System (ROMS)
dc.typeArticle


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