Ice jams emerge from the accumulation of fragmented ice on a specific section of a river, obstructing the channel and restricting the flow. The resulting floods are socioeconomically costly as well as life threatening. When breakup occurs and ice starts to move downstream the river, a key question is, where would the released ice be susceptible to jam? The goal of this work was to develop a simplified geospatial model to estimate the predisposition of a river channel to ice jams.
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Leibniz University Hannover
Institute of Photogrammetry and GeoInformation
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