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New flow relaxation mechanism explains scour fields at the end of submarine channels
Particle-laden gravity flows, called turbidity currents, flow through river-like channels across the ocean floor. These submarine channels funnel sediment, nutrients, pollutants and organic carbon into ocean basins and can extend for over 1000’s of kilometers. Upon reaching the end of these channels...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2019
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6764982/ https://www.ncbi.nlm.nih.gov/pubmed/31562328 http://dx.doi.org/10.1038/s41467-019-12389-x |