Articles | Volume 39
https://doi.org/10.5194/adgeo-39-27-2014
https://doi.org/10.5194/adgeo-39-27-2014
01 Apr 2014
 | 01 Apr 2014

A theoretical analysis of river bars stability under changing channel width

S. Zen, G. Zolezzi, and M. Tubino

Related authors

Coastal vulnerability assessment: through regional to local downscaling of wave characteristics along the Bay of Lalzit (Albania)
Francesco De Leo, Giovanni Besio, Guido Zolezzi, and Marco Bezzi
Nat. Hazards Earth Syst. Sci., 19, 287–298, https://doi.org/10.5194/nhess-19-287-2019,https://doi.org/10.5194/nhess-19-287-2019, 2019
Short summary

Cited articles

Ashmore, P.: Laboratory modelling of gravel braided stream morphology. Earth Surf. Process. Land., 7, 201–225, 1982.
Ashmore, P.: How do gravel-bed rivers braid? Can. J. Earth Sci., 28, 326–341, 1991.
Bertoldi, W. and Tubino, M.: Bed and bank evolution of bifurcating channels, Water Resour. Res., 41, W07001, https://doi.org/10.1029/2004WR003333, 2005.
Church, M. and Rice, S. P.: Form and growth of bars in a wandering gravel-bed river, Earth Surf. Process. Land., 34, 1422–1432, 2009.
Colombini, M., Seminara, G., and Tubino, M.: Finite-amplitude alternate bars, J. Fluid Mech., 181, 213–232, 1987.
Download