Self-sharpening induces jet-like structure in seafloor gravity currents

Gravity currents are the primary means by which sediments, solutes and heat are transported across the ocean-floor. Existing theory of gravity current flow employs a statistically-stable model of turbulent diffusion that has been extant since the 1960s. Here we present the first set of detailed spat...

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Detalles Bibliográficos
Autores principales: Dorrell, R. M., Peakall, J., Darby, S. E., Parsons, D. R., Johnson, J., Sumner, E. J., Wynn, R. B., Özsoy, E., Tezcan, D.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6437198/
https://www.ncbi.nlm.nih.gov/pubmed/30918255
http://dx.doi.org/10.1038/s41467-019-09254-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6437198/
https://www.ncbi.nlm.nih.gov/pubmed/30918255
http://dx.doi.org/10.1038/s41467-019-09254-2

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