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Large organic debris in streams controls the distribution of aquatic habitats, the routing of sediment through stream systems, and the stability of streambed and banks. Management activities directly alter debris loading by addition or removal of material and indirectly by increasing the probability of debris torrents and removing standing streamside trees. We propose a method to assess the risk of high debris flows based on travel times from debris sources to reach specified areas along stream channels.

Large organic debris in streams controls the distribution of aquatic habitats, the routing of sediment through stream systems, and the stability of streambed and banks. Management activities directly alter debris loading by addition or removal of material and indirectly by increasing the probability of debris torrents and removing standing streamside trees. We propose a method to assess the risk of high debris flows based on travel times from debris sources to reach specified areas along stream channels. The method uses the probability of a downstream debris flow as a function of flow magnitude and duration to quantify the risk of debris flow based on travel time to critical areas. The approach is demonstrated with a case study of a small mountain stream in the California Coast Range Mountains. A debris flow occurred in October 2016, with debris transported down multiple reaches including the main channel. This debris would have been transported to a higher percentage of the reach if the debris had been removed from the stream...

Large organic debris in streams controls the distribution of aquatic habitats, the routing of sediment through stream systems, and the stability of streambed and banks. Management activities directly alter debris loading by addition or removal of material and indirectly by increasing the probability of debris torrents and removing standing streamside trees. We propose a method to assess the risk of high debris flows based on travel times from debris sources to reach specified areas along stream channels. The method uses the probability of a downstream debris flow as a function of flow magnitude and duration to quantify the risk of debris flow based on travel time to critical areas. The approach is demonstrated with a case study of a small mountain stream in the California Coast Range Mountains. A debris flow occurred in October 2016, with debris transported down multiple reaches including the main channel. This debris would have been transported to a higher percentage of the reach if the debris had been removed from the stream before the debris flow. This analysis can be applied to estimate the risk of debris flow for other reach locations and for other debris sources that may contribute to the reach.

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