Andere Kunden interessierten sich auch für
![Metamorphic Processes]( "Metamorphic Processes")
Metamorphic Processes39,99 €![Experimental Investigation and Numerical Modeling of Rock Brittle Failure Behavior under High Stress Conditions]( "Experimental Investigation and Numerical Modeling of Rock Brittle Failure Behavior under High Stress Conditions")
Experimental Investigation and Numerical Modeling of Rock Brittle Failure Behavior under High Stress Conditions86,99 €![Snow-Bound at Eagle's]( "Snow-Bound at Eagle's")
Snow-Bound at Eagle's20,90 €![Chemical and Physical Studies in the Metamorphism of Rocks]( "Chemical and Physical Studies in the Metamorphism of Rocks")
Chemical and Physical Studies in the Metamorphism of Rocks17,90 €![The Story of Snow Crystal]( "The Story of Snow Crystal")
The Story of Snow Crystal38,99 €![Snow Crystals]( "Snow Crystals")
Snow Crystals48,00 €![The Abode of Snow]( "The Abode of Snow")
The Abode of Snow29,90 €
Temperature-gradient metamorphism is one of the dominant processes changing the complex microstructure of natural snow. Although many researchers have examined snow metamorphism, the mutual effect of a temperature gradient with additional advective flow on snow metamorphism has not yet been investigated. In this study, temperature-gradient experiments with saturated advective flow were conducted. Using computer tomography, the threedimensional microstructure of five snow samples was assessed non-destructively. The dynamically changing microstructural snow properties, namely the porosity and the specific surface area were determined out of the reconstructed snow volume. The experiments were conducted in the cold laboratories of the WSL Institute for Snow and Avalanche Research SLF in Davos, Switzerland.