Adjustments in river channel geometry as
β
Gurnell, Angela M.
π
Article
π
1997
π
John Wiley and Sons
π
English
β 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