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dc.contributor.authorToft, Håvard B.
dc.contributor.authorMüller, Karsten
dc.contributor.authorHendrikx, Jordy
dc.contributor.authorJaedicke, Christian
dc.contributor.authorBühler, Yves
dc.date.accessioned2023-06-02T07:18:56Z
dc.date.available2023-06-02T07:18:56Z
dc.date.created2023-05-10T09:48:46Z
dc.date.issued2023
dc.identifier.citationCold Regions Science and Technology. 2023, 211 .
dc.identifier.issn0165-232X
dc.identifier.urihttps://hdl.handle.net/11250/3069706
dc.description.abstractAccurate prediction of snow avalanche runout-distances in a deterministic sense remains a challenge due to the complexity of all the physical properties involved. Therefore, in many locations including Norway, it has been common practice to define the runout distance using the angle from the starting point to the end of the runout zone (α-angle). We use a large dataset of avalanche events from Switzerland (N = 18,737) acquired using optical satellites to calculate the α-angle for each avalanche. The α-angles in our dataset are normally distributed with a mean of 33° and a standard deviation of 6.1°, which provides additional understanding and insights into α-angle distribution. Using a feature importance module in the Random Forest framework, we found the most important topographic parameter for predicting α-angles to be the average gradient from the release area to the β-point. Despite the large dataset and a modern machine learning (ML) method, we found the simple linear regression model to yield a higher performance than our ML attempts. This means that it is better to use a simple linear regression in an operational context
dc.language.isoeng
dc.titleCan big data and random forests improve avalanche runout estimation compared to simple linear regression?
dc.title.alternativeCan big data and random forests improve avalanche runout estimation compared to simple linear regression?
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersion
dc.source.pagenumber17
dc.source.volume211
dc.source.journalCold Regions Science and Technology
dc.identifier.doi10.1016/j.coldregions.2023.103844
dc.identifier.cristin2146676
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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