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Influence of channel geomorphic units on bedload transport and river morphology during low‐magnitude bed‐forming floods coupled with sediment augmentation

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By Christian Mörtl, Robin Schroff, Severin Stähly, Geopraevent AG
| Wiley Online Library Verified
esp5635-sup-0001-FigS1.pdfPDF document, 29.8 KB Figure S1. Graph of the rating curve at the measurement location, based on eight calibration points. The variable L is the water level elevation and Q is the discharge. Calibration points are plotted as black dots. esp5635-sup-0002-FigS4.pdfPDF document, 20 KB Figure S4. Graph of the sensitivity of the grainsize parameters for the calculation of the total bedload transport capacity of Flood 2016.
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