Analyses of intermittent mixing and stratification within the North Passage of the Changjiang (Yangtze) River estuary, China: A three-dimensional model study
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文摘

Both longitudinal and lateralϕ-advections are intermittent at the North Passage in the Changjiang River estuary.

Large lateralϕ-advection may be enhanced by large lateral gradient of ϕ there.

Large longitudinal depth-mean straining overlays the effects of tidal straining, circulation and river discharge there.

Large lateral depth-mean straining may be generated by large lateral density gradient interacting with the shear flow there.

Longitudinal non-mean straining, lateral non-mean straining and vertical advection are relatively smaller there.

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