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    Performance of Snow Fence at Banihal Top in Himalayan Region

    Source: Journal of Cold Regions Engineering:;2015:;Volume ( 029 ):;issue: 004
    Author:
    Ganesh Kumar
    DOI: 10.1061/(ASCE)CR.1943-5495.0000088
    Publisher: American Society of Civil Engineers
    Abstract: A continuous snow fence of 50% porosity, 130 m in length, and 4.0 m height was installed to overcome the snowdrift problems at Banihal Top (Jammu and Kashmir, India) in the Himalayan region. The avalanche sites, which affect the north and south Portals of the Jawahar Tunnel, have catchment areas near Banihal Top. The width of mountainous ridge at this site is about 60 m except within a central depression area where the width is about 200–250 m. Snow mass is eroded from the southern windward slope and deposited on the northern leeward slope toward the Kashmir valley during the winter. The rates of erosion and deposition of snow are controlled by snow characteristics, the snow surface roughness, terrain features, and the snow fence configuration. The snow at Banihal Top is wet in nature and snow deposition due to snow drifting is found to be about
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      Performance of Snow Fence at Banihal Top in Himalayan Region

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    contributor authorGanesh Kumar
    date accessioned2017-05-08T22:30:37Z
    date available2017-05-08T22:30:37Z
    date copyrightDecember 2015
    date issued2015
    identifier other47595480.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/81770
    description abstractA continuous snow fence of 50% porosity, 130 m in length, and 4.0 m height was installed to overcome the snowdrift problems at Banihal Top (Jammu and Kashmir, India) in the Himalayan region. The avalanche sites, which affect the north and south Portals of the Jawahar Tunnel, have catchment areas near Banihal Top. The width of mountainous ridge at this site is about 60 m except within a central depression area where the width is about 200–250 m. Snow mass is eroded from the southern windward slope and deposited on the northern leeward slope toward the Kashmir valley during the winter. The rates of erosion and deposition of snow are controlled by snow characteristics, the snow surface roughness, terrain features, and the snow fence configuration. The snow at Banihal Top is wet in nature and snow deposition due to snow drifting is found to be about
    publisherAmerican Society of Civil Engineers
    titlePerformance of Snow Fence at Banihal Top in Himalayan Region
    typeJournal Paper
    journal volume29
    journal issue4
    journal titleJournal of Cold Regions Engineering
    identifier doi10.1061/(ASCE)CR.1943-5495.0000088
    treeJournal of Cold Regions Engineering:;2015:;Volume ( 029 ):;issue: 004
    contenttypeFulltext
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