2023
DOI: 10.1016/j.coldregions.2022.103706
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Fountain scheduling strategies for improving water-use efficiency of artificial ice reservoirs (Ice stupas)

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Cited by 3 publications
(4 citation statements)
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“…Distances between layers vary between 20 and 50 m. The trapping structure itself does not add additional risk in case it is destroyed during an avalanche event, as it does not add any rolling mass. If the site for avalanche trapping is found and selected at an altitude of around 4000 m a.s.l., it can be expected that some of the condensed snow mass will remain and can grow with subsequent snowfall and avalanches, hence producing a permanent mass that could be referred to as an artificial glacier, as in previous attempts using means to create such bodies of ice with water fountains (Balasubramanian et al, 2023).…”
Section: Avalanches and Irrigationmentioning
confidence: 98%
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“…Distances between layers vary between 20 and 50 m. The trapping structure itself does not add additional risk in case it is destroyed during an avalanche event, as it does not add any rolling mass. If the site for avalanche trapping is found and selected at an altitude of around 4000 m a.s.l., it can be expected that some of the condensed snow mass will remain and can grow with subsequent snowfall and avalanches, hence producing a permanent mass that could be referred to as an artificial glacier, as in previous attempts using means to create such bodies of ice with water fountains (Balasubramanian et al, 2023).…”
Section: Avalanches and Irrigationmentioning
confidence: 98%
“…Combining the available database of events with past regional climate data would allow one to understand climatologies of avalanches in HMA better, an approach already employed in the Alps (Eckert et al, 2010). This could allow for a better understanding of the link between a changing climate and the occurrence of avalanches, so far only investigated for a field site in India (Ballesteros-Cánovas et al, 2018) and one in China (Hao et al, 2023). More recently, distributed datasets on a number of variables including snow cover (Muhammad and Thapa, 2021), snow depth (Lievens et al, 2019), snow water equivalent (Smith and Bookhagen, 2018;Liu et al, 2021) and, locally, refreezing within the snowpack (Veldhuijsen et al, 2022) have become available.…”
Section: Avalanche Incidents and Impactsmentioning
confidence: 99%
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“…If the site for avalanche trapping is found and selected at an altitude of around 4000 m a.s.l., it can be expected that some of the condensed snow mass will remain and can grow with subsequent snowfall and avalanches, hence producing a permanent mass that could be referred to as an artificial glacier, as in previous attempts using means to create such bodies of ice with water fountains (Balasubramanian et al, 2023). Moreover, FOCUS has also sourced an avalanche expert to help develop short and medium-term plans to mitigate the risk of avalanches in the highest-risk areas (Chabot and Kaba, 2016).…”
Section: Avalanches and Irrigationmentioning
confidence: 99%