Talus and its cooling effects on the thermal regime of permafrost: A review
Shengtao Lan,
Bin Cao,
Yan Hu
et al.
Abstract:Talus, as the product of movement and accumulation along the slope after the cracking of cliffs or steep rock walls, is a common landform in the mountain periglacial environment. Significant thermal anomalies within talus have been widely reported to be a result of cooling effects. During the cold season, the increased temperature difference between talus and the ambient environment strengthens the intensity of convection (vertical flows) and transforms into upward advection (lateral flows) and exhausts the in… Show more
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