Abstract
The propagation of a periodic thermal wave into snow is signifciantly altered by the presence of a shallow rock interface because of the large difference in thermal properties of the two media. The temperature distribution is modeled using classical heat conduction equations subject to a periodic diurnal or seasonal surface heat flux conditions, jump conditions at the interface, and insulating conditions in the far-field. The resuls show that during a period of atmospheric cooling the presence of a buried rocky outcrop increases the snow temperature and temperature gradients simultaneously to produce very favorable conditions for crystal growth and avalanche formation. -Authors
| Original language | English |
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| Pages (from-to) | 15-279 |
| Number of pages | 264 |
| Journal | Journal of Geophysical Research: Atmospheres |
| Volume | 100 |
| Issue number | 8 |
| Publication status | Published - 1995 |