Formation of spiky structures in high-altitude snow patches: penitente tilting

Pablo Guilleminot; Rodrigo Olea

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arXiv · 1804.09700

Formation of spiky structures in high-altitude snow patches: penitente tilting

Pablo Guilleminot·Rodrigo Olea

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Abstract

Penitentes are spikes formed on the surface of the snow, which are present typically at high altitude in the Andes and Himalayas. They are a consequence of a thermodynamic instability, as a result of the surface sublimation at a given point due to the incidence of light scattered by surrounding features. Here, based on existing literature, we model the time evolution of penitente formation as a purely radiation-driven phenomenon. The physical system is governed by a 1D diffusion equation with a nonlocal source term, which represents the light coming in from all the line of sight accessible from that point of the curve. For small perturbations on the initial profile, the surface undergoes an instability which triggers the formation of spiky structures. For solar radiation coming in the surface at a given angle, our numerical simulations account for a feature observed in the real system: penitentes get tilted in the direction of the sunlight.

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Pablo Guilleminot, Rodrigo Olea. 2018-04-25. Formation of spiky structures in high-altitude snow patches: penitente tilting. https://arxiv.org/abs/1804.09700

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