𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Reach-scale channel geometry of a mountain river

✍ Scribed by Ellen Wohl; Jessica N. Kuzma; Nancy E. Brown


Publisher
John Wiley and Sons
Year
2004
Tongue
English
Weight
228 KB
Volume
29
Category
Article
ISSN
0360-1269

No coin nor oath required. For personal study only.


πŸ“œ SIMILAR VOLUMES


Describing scales of features in river c
✍ Nestler, John ;Sutton, Virginia K. πŸ“‚ Article πŸ“… 2000 πŸ› John Wiley and Sons 🌐 English βš– 595 KB

Quantitative description of spatial patterns is often at the heart of ecological research in aquatic systems, particularly for investigations of how biota respond to physical habitat. A common first step for approximating a river channel is tessellation, or the discretization of the channel into cel

A reach-scale biogeochemical model for t
✍ Ourania Tzoraki; Nikolaos P. Nikolaidis; Anna Rosa Trancoso; Frank Braunschweig; πŸ“‚ Article πŸ“… 2009 πŸ› John Wiley and Sons 🌐 English βš– 272 KB

## Abstract The RS‐tempQ Model (**r**each–**s**cale **t**emporary flow biogeochemical model) is a conceptual model that can describe the hydrologic, sediment transport and biogeochemical processes of temporary rivers at the reach scale. The model takes into account the expansion–contraction of the

Adjustments in river channel geometry as
✍ Gurnell, Angela M. πŸ“‚ Article πŸ“… 1997 πŸ› John Wiley and Sons 🌐 English βš– 671 KB

Major hydraulic discontinuities along lowland rivers may be caused by water impoundment behind weirs, by tributary floods, and by tides. An analysis of the geometry of 122 surveyed channel cross-sections located on an 18 km reach of the lower River Dee identifies up to three levels in the bank profi