In the last 30 years, work on large wood (LW) has expanded and matured considerably, and
river scientists, managers and practitioners now have a better appreciation of the role of LW …

Different models have been used in science and practice to identify instream large-wood
(LW) sources and to estimate LW supply to rivers. This contribution reviews the existing …

Macroplastic storage in mountain rivers remains unexplored and it is unknown how river
morphology and different surface types of river areas modulate this process. Therefore, we …

Porosity, or void space, of large wood jams in stream systems has implications for estimating
wood volumes and carbon storage, the impacts of jams on geomorphic and ecological …

Abstract We use Google Earth imagery, drone imagery, and ground-based field
measurements to assess the abundance, spatial distribution, and size of accumulations of …

Large wood (LW) can be transported along a river during floods, increasing flood‐
associated hazards, particularly when it accumulates at river‐spanning infrastructures such …

Large wood (LW) commonly forms log jams, influencing bed composition and biota via
complex flow-sediment-wood interactions. A LW blockage, often induced by river-crossing …

Log jams alter gradients in hydraulic head, increase the area available for hyporheic
exchange by creating backwater areas, and lead to the formation of multiple channel …

Quantification and assessment of large wood (LW) accumulations in fluvial systems is still
considered difficult due to the complex nature of wooden deposits. Although knowledge …

Valley bottom process reset, or the excavation of high surfaces and fill of incised channels
combined with large wood addition, is a new method for creating multi-channel river-wetland …