Zobrazeno 1 - 10
of 15
pro vyhledávání: '"A. I. Mears"'
Publikováno v:
The Technical Avalanche Protection Handbook
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::357a815873255f073f424a324f90e687
https://doi.org/10.1002/9783433603840
https://doi.org/10.1002/9783433603840
Autor:
D. M. Mcclung, A. I. Mears
Publikováno v:
Journal of Glaciology. 41:359-372
The prediction of run-up and run-out of dry-flowing avalanches is very important for land-use planning, design of run-out zone defenses and construction of risk maps in avalanche terrain. In this paper, we present a numerical dynamics model to predic
Autor:
A. I. Mears, David M. McClung
Publikováno v:
Journal of Glaciology. 41:359-372
The prediction of run-up and run-out of dry-flowing avalanches is very important for land-use planning, design of run-out zone defenses and construction of risk maps in avalanche terrain. In this paper, we present a numerical dynamics model to predic
Autor:
A. I. Mears, David M. McClung
Publikováno v:
Cold Regions Science and Technology. 19:163-175
Avalanche runout distances have traditionally been calculated by selecting friction coefficients and then using them in an avalanche dynamics model. Uncertainties about the mechanical properties of flowing snow and its interaction with terrain make t
Publikováno v:
Annals of the Association of American Geographers. 66:129-144
Interdisciplinary field studies and remote sensing techniques were used to delineate mountain areas in Colorado subject to such natural hazards as snow avalanches, mudflows, rockfalls, and landslides. The old mining townsite of Ophir in the northwest
Autor:
W. C. Bradley, A. I. Mears
Publikováno v:
GSA Bulletin. 91:1057-1090
Publikováno v:
Journal of Glaciology. 26:109-119
The friction coefficients needed to solve Voellmy’s avalanche-dynamics equations and as input to the numerical, finite-difference computer program AVALNCH are calculated from case studies. The following coefficients of internal friction v and of su
Autor:
Arthur I. Mears
Publikováno v:
Journal of Glaciology. 26:153-163
Field data on dry–slab avalanches obtained during the period 1975–79 from several snow climates suggest the following: (1) most of the mass of the typical avalanche studied consisted of fragments with lengths greater than 5 cm, (2) transverse and