Impact of Changing Concavity Indices on Channel Steepness and Divide Migration Metrics
Boris Gailleton, Simon M. Mudd, Fiona J. Clubb, Stuart Grieve, Martin D. Hurst
Abstract
Abstract The concavity index, , describes how quickly river channel gradient declines downstream. It is used in calculations of normalized channel steepness index, , a metric for comparing the relative steepness of channels with different drainage area. It is also used in calculating a transformed longitudinal coordinate, , which has been employed to search for migrating drainage divides. A value of 0.45 is typically assumed in studies. Here we quantify the variability in across multiple landscapes distributed across the globe. We describe the degree to which both the spatial distribution and magnitude of and can be distorted if is assumed rather than constrained. Differences between constrained and assumed of 0.1 or less are unlikely to affect the spatial distribution and relative magnitude of values, but larger differences can change the spatial distribution of and in extreme cases invert differences in relative steepness: relatively steep reaches can appear relatively gentle as quantified by . These inversions are function of the range of drainage area in the considered watersheds. We also demonstrate that the coordinate, and therefore the detection of migrating drainage divides, is sensitive to varying values of . The median of most likely across a wide range of mountainous and upland environments is 0.425. This wide range of variability suggests workers should not assume any value for , but should instead calculate a representative for the landscape of interest, and exclude basins for which this value is a poor fit.