The different flow regimes of an open channel flow including a hydraulic jump. fluidsin4k
Dye streaks are used to demonstrate the dynamics of rotating flow in the midlatitude ocean. Photo: R. Griffiths.
Convective flow produced when a fluid is uniformely injected inderneath a denser and much more viscous fluid.Photo: M. Jellinek
Holmboe instability propagates along a stratified inteface. Photo A. Hogg.
A laboratory simulation of mantle plume. Photo R. Griffiths.
Schlieren image of internal gravity waves radiating froma source. Photo: B. Ruddick.
Wax is used to model freezing lava flow down a slope. Photo: R. Kerr, K. Cashman, R. Griffiths.
Colour Schlieren image of a long internal wave breaking on a slope. Photo: Greg Ivey.
A series of photos showing different behaviour of lava domes as a function of lava rheology. Photo: R. Griffiths.
Flow of dense water over a still creates turbulence of the downstream side. Photo: T. Prastowo.
A Kelvin-Helmholtz billow. Photo A. Hogg.