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Soft transition between subcritical and supercritical currents through intermittent cascading interfacial instabilities

Long-running gravity currents are flows that are submerged beneath a deep layer of quiescent fluid and they travel over long distances along inclined or horizontal surfaces. They are driven by the density difference between the current and the clear ambient fluid above. In this work we present resul...

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Détails bibliographiques
Publié dans:Proc Natl Acad Sci U S A
Auteurs principaux: Salinas, Jorge, Balachandar, S., Shringarpure, Mrugesh, Fedele, Juan, Hoyal, David, Cantero, Mariano
Format: Artigo
Langue:Inglês
Publié: National Academy of Sciences 2020
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC7414079/
https://ncbi.nlm.nih.gov/pubmed/32690702
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2008959117
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