Jens M. Turowski

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[1] Steep mountain streams typically feature macro-roughness elements like boulders, step-pool sequences, and a varying channel width. Flow resistance because of such roughness elements appears to be an important control on bedload transport rates. Many commonly used bedload transport equations overestimate the transport in steep streams by orders of(More)
Climate change influences air temperature and precipitation, and as a direct consequence, the annual discharge pattern in rivers will change as climate warming continues. This has an impact on bedload transport and consequently on aquatic life, because coarse sediments in streams provide important habitat for many species. Salmonids, for example, spawn in(More)
Due to an unfortunate turn of events, incorrect versions of Figs. 5, 6, 7, and 8 were used in the above-mentioned publication. These figures show the results using a now outdated version of the model sedFlow. The text of the original article refers to the proper results produced with the final version of the model. The four figures including their correct(More)
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