detrainment of a gravity current into linear stratification from a 45 degree slope.

Note the significant detrainment that occurs over the whole depth. Related dynamics are described in research paper at

Marques, G. M., Wells, M. G., Padman, L., & Özgökmen, T. M. (2017). Flow splitting in numerical simulations of oceanic dense-water outflows. Ocean Modelling, 113, 66-84.

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