2018
DOI: 10.1029/2018wr022819
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Finite Amplitude of Free Alternate Bars With Suspended Load

Abstract: River bars are macroscale sediment patterns, whose main geometrical features (wavelength and amplitude) depend on the mutual interactions between hydrodynamics and sediment transport. River bars develop as an instability of the plane bed to an infinitesimal perturbation, which grows in time to eventually reach a finite amplitude. We here determine, with reference to both bed and suspended loads, a closed form for the finite amplitude, through the nonlinear Center Manifold Projection technique. Results show tha… Show more

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Cited by 28 publications
(41 citation statements)
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“…gives rise to the second-order, A 00 , A 02 A 20 , A 22 harmonics (see Colombini et al, 1987;Bertagni and Camporeale, 2018).…”
Section: The Alternate Nature Of Both Alternate Bars and Diagonal Barsmentioning
confidence: 99%
“…gives rise to the second-order, A 00 , A 02 A 20 , A 22 harmonics (see Colombini et al, 1987;Bertagni and Camporeale, 2018).…”
Section: The Alternate Nature Of Both Alternate Bars and Diagonal Barsmentioning
confidence: 99%
“…This suggests δp=false[U0D0/false(wsλfalse)false] to be much smaller than unity. As the δp depends on the priori unknown wavelength of riverbed-patterns, we define another small parameter δ as δ=δpλ/B=U0/false(βwsfalse) [30,32].…”
Section: Theoretical Analysis Of Particle Transportmentioning
confidence: 99%
“…Substituting equations (4.1)–(4.4) into equations (2.3)–(2.5) and (3.6), we obtain L0normal∂bold-italicVfalse^normal∂t=Lmbold-italicVfalse^+boldNfalse(bold-italicVfalse^false)+Ofalse(V^3false), where L0 is the 4×4 matrix whose elements are zero except the lower right entry (being equal to unity), Lm is the 4×4 matrix differential operator and the term Nfalse(bold-italicVfalse^false) contains all the second-order nonlinearities. The perturbations can be expanded in terms of the eigenfunctions as follows [32,50]: bold-italicVfalse^false(x,y,tfalse)=.2em0.333emp=p0p=normal∞m=1nA...…”
Section: Stability Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…Specifically, there is not an upper limit of the Shields number for the formation of alternate bars. As a consequence, alternate bars are definitely expected to form in sand bed rivers (e.g., Bertagni and Camporeale, 2018), often coexisting with dunes, as also highlighted by the Referee #1.…”
mentioning
confidence: 93%