Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Gaetano Porcile"'
Publikováno v:
Communications Earth & Environment, Vol 1, Iss 1, Pp 1-13 (2020)
Intense rip currents caused by tropical cyclones can drive sediment-laden turbidity flows down submarine canyons, according to numerical simulations. Shoreline shape, bathymetry and incoming wave direction are key factors controlling this phenomenon.
Externí odkaz:
https://doaj.org/article/8002fad391f14ee4ace6590f277f40c6
Publikováno v:
Journal of geophysical research: Earth surface, 128(1):e2022JF006796. Wiley-Blackwell
The formation of fluvial dunes is usually studied by investigating the time development of a small amplitude bottom perturbation of a uniform stream and considering that the dunes originate by the growth of the bottom mode characterized by the larges
Publikováno v:
Applied Ocean Research. 137:103602
Publikováno v:
ISSUE=679;TITLE=EGU General Assembly 2021
Field observations in the Dover Strait (Le Bot and Trentesaux, 2004) show sandy bed patterns in an environment where sand is scarce. Their morphological features closely resemble tidal sand waves, however, these type of bed forms are characterized by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de9e35ca82b7b3866df3f1b4a4a9201b
https://doi.org/10.5194/egusphere-egu21-16019
https://doi.org/10.5194/egusphere-egu21-16019
Publikováno v:
Applied Ocean Research. 121:103085
Publikováno v:
Communications Earth & Environment, Vol 1, Iss 1, Pp 1-13 (2020)
Tropical cyclones impose stresses on narrow and shallow continental shelves. The interaction of strong wind- and wave-induced currents with the local topography near the shore gives rise to complex flow and sediment transport patterns. Considerable u
When narrow continental shelves are stressed by extreme weather events, nearshore currents dominate the coastal circulation leading to complex flow patterns that can result in previously unforeseen cross-shelf exchange of water and sediment. Here we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::569de7ab2764f01ea64f23c234348873
https://doi.org/10.5194/egusphere-egu2020-20168
https://doi.org/10.5194/egusphere-egu2020-20168
Publikováno v:
Coastal Engineering. 141:12-23
We investigate the turbulent oscillatory flow generated by propagating surface waves close to the sea bottom focusing our attention on moderate values of the Reynolds number R δ of the bottom boundary layer. For such moderate values of R δ , turbul