2018
DOI: 10.1007/s11069-018-3457-y
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Calculating snow-avalanche return period from tree-ring data

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Cited by 11 publications
(5 citation statements)
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“…Overall, this study region provides an ideal natural setting for studying avalanches due to its geography, inclusion of transportation and recreation corridors potentially impacted by avalanches, relative accessibility, and no artificial avalanche hazard mitigation. Northwest Montana's avalanche climate is classified as both a coastal transition and intermountain avalanche climate (Mock and Birkeland, 2000), but it can exhibit characteristics of both continental and coastal climates. The elevation of avalanche paths within the study sites range from approximately 1100 to 2700 m, and the starting zones of these paths are distributed among all aspects (Table 1).…”
Section: Study Sitementioning
confidence: 99%
“…Overall, this study region provides an ideal natural setting for studying avalanches due to its geography, inclusion of transportation and recreation corridors potentially impacted by avalanches, relative accessibility, and no artificial avalanche hazard mitigation. Northwest Montana's avalanche climate is classified as both a coastal transition and intermountain avalanche climate (Mock and Birkeland, 2000), but it can exhibit characteristics of both continental and coastal climates. The elevation of avalanche paths within the study sites range from approximately 1100 to 2700 m, and the starting zones of these paths are distributed among all aspects (Table 1).…”
Section: Study Sitementioning
confidence: 99%
“…Finally, the temporal reconstruction and spatial extent of the avalanche winters have been obtained in the three avalanche paths investigated. The return intervall (or return period) considered as being the average interval of time within which the runout distance is reached by snow avalanches or exceeded at a given location (McClung and Schaerer 2006;Meses ¸an et al, 2018) was calculated by dividing the time interval (in years) of the tree-ring reconstructed snow-avalanche chronology by the number of snow avalanches events recorded during this period (Boucher et al, 2003). For each of three paths investigated, the average return intervalls at the scale of the entire snow-avalanche path were obtained.…”
Section: Tree-ring Methodsmentioning
confidence: 99%
“…But once it happens, it will cause great damage to the distribution network. The frequency of suffering from extreme disasters in an area can be measured by the return period [20]. The return period refers to the average number of time intervals between repeated occurrences of an event in many trials.…”
Section: Resiliencementioning
confidence: 99%
“…where 𝜇 is mathematical expectations, 𝜎 2 is variance. In summary, the constraints of the PV-ES-CSs are as follows: (20) where P ES is charging and discharging power of ES. P ES_min and P ES_max are lower and upper limits of charging and discharging power for ES.…”
Section: Constraint Conditionmentioning
confidence: 99%