Systematic valley floor extraction for characterizing valley width distribution in mountain landscapes : comparison between hydraulic and geometrical approaches
Abstract. Valleys are key elements of mountainous landscapes, governing the transfer of water and sediment while recording the influence of tectonic and climatic forcing. Despite their importance, the quantitative characterization of valley morphology at large spatial scales remains challenging, particularly due to limitations in automated extraction methods. In this study, we compare two approaches for delineating valley extent from digital elevation models: a classical geometrical method based on topographic thresholds, and a novel pseudo-hydraulic method that estimates flood-prone areas using a simplified water-filling algorithm. Using 30 m resolution DEMs, we find that both perform well and that the conceptual difference between them is mainly significant in headwater areas. We then find that the main control on valley width is drainage area, consistent with previous work. The use of a wideness index allows us to identify local deviations from the width–area scaling, highlighting secondary controls such as lithological changes. New insights into valley morphology could be obtained through the large-scale systematic extraction of valleys across various tectonic and climatic settings.
This manuscript investigates two automated tools for quantifying valley width and tests them in far-flung field study area to deduce systematic trends in valley width as well as factors that cause valley width to deviate from these trends. The authors develop a novel, flood-based algorithm that uses a hydraulic-like approach and compare it to a geometric approach previously developed and published by the authors. They test these algorithms using geologic maps of alluvial deposits and use a statistical approach to assess performance. Their findings confirm previous studies showing how valley width tends to scale with drainage area and they also show how tectonics, glacial history, and bedrock affects valley width. The wideness index is a clever and useful tool that has much promise. The manuscript is generally well-written with thorough scholarship and novel observations. The manuscript is very well-suited for ESURF and should be published after some minor revisions detailed below.
minor comments:
line 39: "first" appears, but "second" does not. Also, this would be better structured as one paragraph.
line 53: these "other controls" are relatively unsatisfying. can the authors explain a bit more about how these processes feedback on valley width and how it may affect observed trends?
line 55: do the authors mean "channel" profiles? the vast lectures on tectonic geomorph focuses on channel profiles.
line 137-9: incomplete sentence and inconsistent structure. rewrite for clarity.
line 297: "that" not "the"
line 344-6: refer to the figures that show these trends.
line 380-6: make one paragraph.
line 392: distributions
line 396-7: the choice and method of separating up and down stream valleys with a 300m threshold is not clear. how does this work? please refer to a figure and show what's being done. also, is this choice driven by the scottish highlands? can this be more systematic?