Resonant and near-resonant internal wave triads for non-uniform stratifications. Part 2. Vertically bounded domain with mild-slope bathymetry
S Gururaj, A Guha - Journal of Fluid Mechanics, 2022 - cambridge.org
Weakly nonlinear internal wave–wave interaction is a key mechanism that cascades energy
from large to small scales, leading to ocean turbulence and mixing. Oceans typically have a …
from large to small scales, leading to ocean turbulence and mixing. Oceans typically have a …
[PDF][PDF] Energy cascade of internal gravity waves in oceans
S Gururaj - 2023 - discovery.dundee.ac.uk
Meridional Overturning Circulation (MOC) is a system of ocean currents spanning thousands
of kilometers transporting heat, salt, carbon, and nutrients to different parts of the ocean. A …
of kilometers transporting heat, salt, carbon, and nutrients to different parts of the ocean. A …
Sensitivity of internal wave energy distribution over seabed corrugations to adjacent seabed features
F Karimpour, A Zareei, J Tchoufag… - Journal of Fluid …, 2017 - cambridge.org
Here we show that the distribution of energy of internal gravity waves over a patch of seabed
corrugations strongly depends on the distance of the patch to adjacent seafloor features …
corrugations strongly depends on the distance of the patch to adjacent seafloor features …
[PDF][PDF] Energy transfer in resonant and near-resonant internal wave triads for non-uniform stratifications. Part 2: Bounded domain with mild-slope bathymetry
S Gururaj, A Guha - arXiv e-prints, 2021 - researchgate.net
Weakly nonlinear internal wave-wave interaction is a key mechanism that cascades energy
from large to small scales, leading to ocean turbulence and mixing. Oceans typically have a …
from large to small scales, leading to ocean turbulence and mixing. Oceans typically have a …