ABSTRACT. The tensile strength (rupture modulus) of new snow layers was measured at a 3,200m elevation Colorado site during February and March, 1998 to determine a) if the cantilever-beam test produced consistent results within a layer at a given time and b) to measure the change in strength over a period of days. 80 tests were conducted on 16 layers by calculating tensile strength at ruptureon cantilever beams 10 to 16 cm thick which were excavated into the new snow. The strength tests a) produced reasonably consistent results, and b) indicated a substantial increase in tensile strength within the snow layers tested during a period of 2 to 4 days after a fresh snowfall. Two periods of widespread, natural soft-slab avalanches occurred in th...
ABSTRACT: Recent experimental and theoretical work has provided new insight into weak layer fracture...
ABSTRACT. The release of a dry-snow slab avalanche involves brittle fracture. It is therefore essent...
Deep slab avalanches are often initiated by the catastrophic collapse of a weak basal layer under th...
Experimental procedure and measured estimates of the tensile strength of snow are given by a new met...
Fracture mechanics has been applied for over 30 years to explain the release of slab avalanches, but...
ABSTRACT: There is a lack of measurements on the rapidly changing mechanical and physical propertie...
Abstract. Knowledge about snow mechanics and snow avalanche formation forms the basis of any hazard ...
If a weak snow layer below a cohesive slab is present in the snow cover, unstable snow conditions ca...
Snow as a construction material has been used for centuries, with igloos among the first examples. E...
Dry-snow slab avalanches start with a failure in a weak snow layer below a cohesive snow slab of amp...
Researchers and practitioners have long utilized a variety of penetrometers to investigate the snowp...
Avalanche occurrence is closely related to the local meteorological conditions which may be quite va...
ABSTRACT: Near-surface warming by either an increase in air temperature or radiation is believed to ...
ABSTRACT: Researchers and practitioners have long utilized a variety of penetrometers to investigat...
Abstract- It is known that snow metamorphism is initially. en by the tendency of individual snow gra...
ABSTRACT: Recent experimental and theoretical work has provided new insight into weak layer fracture...
ABSTRACT. The release of a dry-snow slab avalanche involves brittle fracture. It is therefore essent...
Deep slab avalanches are often initiated by the catastrophic collapse of a weak basal layer under th...
Experimental procedure and measured estimates of the tensile strength of snow are given by a new met...
Fracture mechanics has been applied for over 30 years to explain the release of slab avalanches, but...
ABSTRACT: There is a lack of measurements on the rapidly changing mechanical and physical propertie...
Abstract. Knowledge about snow mechanics and snow avalanche formation forms the basis of any hazard ...
If a weak snow layer below a cohesive slab is present in the snow cover, unstable snow conditions ca...
Snow as a construction material has been used for centuries, with igloos among the first examples. E...
Dry-snow slab avalanches start with a failure in a weak snow layer below a cohesive snow slab of amp...
Researchers and practitioners have long utilized a variety of penetrometers to investigate the snowp...
Avalanche occurrence is closely related to the local meteorological conditions which may be quite va...
ABSTRACT: Near-surface warming by either an increase in air temperature or radiation is believed to ...
ABSTRACT: Researchers and practitioners have long utilized a variety of penetrometers to investigat...
Abstract- It is known that snow metamorphism is initially. en by the tendency of individual snow gra...
ABSTRACT: Recent experimental and theoretical work has provided new insight into weak layer fracture...
ABSTRACT. The release of a dry-snow slab avalanche involves brittle fracture. It is therefore essent...
Deep slab avalanches are often initiated by the catastrophic collapse of a weak basal layer under th...