Fig. 1: Numerical experiments.
From: Different geomorphic processes control suspended sediment and bedload export from glaciers
a Cartoon of subglacial processes considered in the model, with inverted parameters noted sediment production rate (\(\dot{\varepsilon }\)), the sediment height initial condition (H0), the channel shape (β), and channel roughness (fi); channel cross section modified from Delaney et al.54 b Bedload and suspended load in a subglacial channel with ice above. c Map of Otemma glacier with the star denoting measurement station location and blue outline of glacier. Image from SwissTopo.
