Layer-average turbidity models lose their range of validity and, besides, may generate instabilities when the concentration of suspended material in the hyperpycnal tongue is highly reduced due to deposit (as r=rho_1/rho_2 approx 1).

If you have expertise on this subject, how would you model these effects in a turbidity current model?

Important item: one thing is what it really happens in nature, and another different thing is how to effectively model this.

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