Wind-tunnel study of snowdrift around avalanche defence structures

被引:1
作者
Jaedicke, C
Naaim-Bouvet, F
Granig, M
机构
[1] Cemagref, F-38402 St Martin Dheres, France
[2] Norwegian Geotech Inst, N-0806 Oslo, Norway
[3] BOKU Wien, A-1180 Vienna, Austria
来源
ANNALS OF GLACIOLOGY, VOL 38, 2004 | 2004年 / 38卷
关键词
D O I
10.3189/172756404781814799
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Avalanche defence structures such as retarding dams and breaking mounds are widely used to protect residential areas and other kinds of infrastructure. The effect of the defence structures depends largely on their effective height relative to the velocity, volume and flow depth of the avalanche. Snow depositions from earlier avalanches as well as from drifting snow can significantly alter the effective height of defence structures. Different designs of avalanche-breaking mounds and retarding dams were tested in the Cemagref (Grenoble, France) wind tunnel for their effect on drifting snow. Examples included dams and mounds of different sizes and heights. The models were tested in a wind tunnel with sand particles subjected to different wind directions. The resulting depositions were scanned with a laser system to obtain a three-dimensional picture of the accumulation pattern. The results show that the accumulated snow varies widely with the design of the structure for a given wind direction. Most snow is accumulated around narrow mounds, with least accumulation observed around mounds covering a smaller relative area of the avalanche path. The data obtained can be used to study the effect of the depositions on the retarding effect of the avalanche defence structures. However, because the similarity criteria for studying the interaction between structures and saltating particles in a wind tunnel cannot be met, the transfer of the results to reality must be performed with caution.
引用
收藏
页码:325 / 330
页数:6
相关论文
共 15 条
[1]   REQUIREMENTS FOR MODELING OF A SNOWDRIFT [J].
ANNO, Y .
COLD REGIONS SCIENCE AND TECHNOLOGY, 1984, 8 (03) :241-252
[2]  
[Anonymous], 1941, PHYS BLOWN SAND DESE
[3]  
Finney E. A., 1939, MICHIGAN STATE COLL, V86
[4]  
HAKONARDOTTIR KM, 2001, VIG01007UR02
[7]   DRIFTING-SNOW SIMILITUDE-TRANSPORT-RATE AND ROUGHNESS MODELING [J].
IVERSEN, JD .
JOURNAL OF GLACIOLOGY, 1980, 26 (94) :393-403
[8]   SNOWDRIFTING - A REVIEW OF MODELING METHODS [J].
KIND, RJ .
COLD REGIONS SCIENCE AND TECHNOLOGY, 1986, 12 (03) :217-228
[9]  
MELLOR M, 1965, CRREL MONOGR
[10]   Study in a climatic wind tunnel (Cryospheric Environment Simulator) of the influence of the type of grain of snow and of the flow on the formation of a snow-drift [J].
Michaux, JL ;
Naaim-Bouvet, F ;
Kosugi, K ;
Sato, A ;
Sato, T .
HOUILLE BLANCHE-REVUE INTERNATIONALE DE L EAU, 2002, (6-7) :79-83