Fig. 5: Aggregated observational data from the 10 trunk channels indicate the non-predictable nature of geomorphic river mobility, with considerable noise in the observational record.
From: Big data show idiosyncratic patterns and rates of geomorphic river mobility
Relationship between (a) active channel width and cross-valley locational probability, (b) valley floor width and cross-valley locational probability and (c) valley floor width and active channel width. A black marker with a plus sign symbology denotes the median. Marginal boxplots show the median and interquartile range; outliers are defined as values more than 1.5 times the interquartile range.
