In a stably stratified shear layer, multiple competing instabilities produce sensitivity to small
changes in initial conditions, popularly called the butterfly effect (as a flapping wing may …

Studies of Kelvin–Helmholtz (KH) instability have typically modelled the initial flow as an
isolated shear layer. In geophysical cases, however, the instability often occurs near …

Physical processes behind flow‐topography interactions and turbulent transitions are
essential for parameterization in numerical models. We examine how the Kuroshio …

With the scarcity of water resources in various regions, the pressure on water supply projects
is also increasing, which has led to a sharp increase in the water hammer effect in water …

Abstract Studies of Kelvin-Helmholtz instability have modelled the initial flow as an isolated
shear layer, without the effects of a no-slip boundary or a neighboring shear layer. However …

Studies of Kelvin–Helmholtz (KH) instability have typically modelled the initial mean flow as
an isolated stratified shear layer. However, geophysical flows frequently exhibit multiple …