Ocean Mixing 2022
DOI: 10.1016/b978-0-12-821512-8.00017-7
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Mixing in equatorial oceans

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Cited by 1 publication
(2 citation statements)
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“…The pronounced overestimation of K T can also be understood from a physical oceanographic perspective. Physically, subject to intense deep-cycle turbulence [ 3 , 6 , 30 ], ocean tracers and momentum are well mixed above the EUC core, leading to a weak stratification and a weak shear in the regions where the training data are measured. In contrast, vertical diffusion is very weak in the ocean interior.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The pronounced overestimation of K T can also be understood from a physical oceanographic perspective. Physically, subject to intense deep-cycle turbulence [ 3 , 6 , 30 ], ocean tracers and momentum are well mixed above the EUC core, leading to a weak stratification and a weak shear in the regions where the training data are measured. In contrast, vertical diffusion is very weak in the ocean interior.…”
Section: Resultsmentioning
confidence: 99%
“…The Pacific equatorial cold tongue is a key region whose sea surface temperature (SST) variations impact worldwide through atmospheric teleconnections. It is widely accepted that oceanic turbulent mixing plays a major role in the equatorial heat budget [ 3 , 4 , 30 ]. However, great uncertainties still exist in the parameterizations of oceanic turbulent mixing [ 7 , 8 , 12 , 33–35 ], which has been a primary source for model biases in ocean and climate modeling.…”
Section: Discussionmentioning
confidence: 99%