Coevolving aerodynamic and impact ripples on Earth
January 8, 2024
Wind-blown sand creates multiscale bedforms on Earth, Mars and other planetary bodies. According to conventional wisdom, decametre-scale dunes and decimetre-scale ripples emerge via distinct mechanisms on Earth: a hydrodynamic instability related to a phase shift between the turbulent flow and the topography and a granular instability related to a synchronization of hopping grains with the topography. [Read more…] about Coevolving aerodynamic and impact ripples on Earth