Zobrazeno 1 - 5
of 5
pro vyhledávání: '"M. I. Cantero"'
Autor:
Jorge S. Salinas, S. Balachandar, M. Shringarpure, J. Fedele, D. Hoyal, S. Zuñiga, M. I. Cantero
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
This study investigates the underlying physical mechanisms of turbidity currents travelling thousands of miles in confined submarine settings, rather than diffusing after short distance. Using high resolution simulations with up to a billion grid poi
Externí odkaz:
https://doaj.org/article/975009e8e6f24cb18dd7a63509d0eeac
Publikováno v:
Earth Surface Dynamics, Vol 2, Iss 2, Pp 419-431 (2014)
Sediment transport in nature comprises of bedload and suspended load, and precise modelling of these processes is essential for accurate sediment flux estimation. Traditionally, non-cohesive suspended sediment has been modelled using the advection–
Externí odkaz:
https://doaj.org/article/656aa51d038c40669d785f77a1a4cafc
Autor:
Jorge S. Salinas, S. Balachandar, Santiago L. Zúñiga, M. Shringarpure, J. Fedele, D. Hoyal, M. I. Cantero
Publikováno v:
Physics of Fluids. 35:016610
Gravity currents are flows driven by the action of gravity over fluids with different densities. Here, we focus on gravity currents where heavier fluid travels along the bottom of a sloping bed, underneath a large body of stagnant lighter ambient flu
Publikováno v:
Journal of Geophysical Research: Oceans. 124:7989-8016
Sediment transport in nature comprises of bed-load and suspended load, and precise modelling of suspended load transport is essential for accurate sediment flux estimation. Traditionally, non-cohesive suspended sediment has been modelled using the ad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f05e26f7974be62bfefddbb77b7ebd0
https://doi.org/10.5194/esurfd-1-923-2013
https://doi.org/10.5194/esurfd-1-923-2013