Physical processes causing the formation of penitentes
arXiv:1511.01725 · doi:10.1103/PhysRevE.92.033015
Abstract
Snow penitentes form in sublimation conditions by differential ablation. Here we investigate the physical processes at the initial stage of penitente growth and perform the linear stability analysis of a flat surface submitted to the solar heat flux. We show that these patterns do not simply result from the self-illumination of the surface --a scale-free process-- but are primarily controlled by vapor diffusion and heat conduction. The wavelength at which snow penitentes emerge is derived and discussed. We found that it is controlled by aerodynamic mixing of vapor above the ice surface.
11 pages, 10 figures
References in corpus (1)
Cited by in corpus (6)
- Penitentes as the origin of the bladed terrain of Tartarus Dorsa, Pluto
- Basal pressure variations induced by a turbulent flow over a wavy surface
- How dirt cones form on glaciers: field observation, laboratory experiments and modeling
- Buoyancy driven dissolution of inclined blocks: Erosion rate and pattern formation
- Onset of glacier tables
- Formation of spiky structures in high-altitude snow patches: penitente tilting