2022
DOI: 10.1016/j.advwatres.2022.104236
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Development of a numerical model for braided river morphology and vegetation evolution with application to the Lower Waitaki River (Aotearoa – New Zealand)

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Cited by 9 publications
(35 citation statements)
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“…Preliminarily, we remark that in this work braided channel evolution is modeled using a mathematical model and numerical solution that are completely deterministic. In detail, the underlying system of governing equations (Equations 1-4 in Stecca et al [2022], see also the electronic supplement to this article) is hyperbolic (Cordier et al, 2011) and thus, with appropriate initial and boundary conditions, can be proven to form a well-posed initialvalue problem that admits a unique solution. Also, the numerical solver employed for this work is deterministic in that two model runs conducted with perfectly identical setups will produce identical results.…”
Section: Results: Display Of Deterministic Chaosmentioning
confidence: 99%
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“…Preliminarily, we remark that in this work braided channel evolution is modeled using a mathematical model and numerical solution that are completely deterministic. In detail, the underlying system of governing equations (Equations 1-4 in Stecca et al [2022], see also the electronic supplement to this article) is hyperbolic (Cordier et al, 2011) and thus, with appropriate initial and boundary conditions, can be proven to form a well-posed initialvalue problem that admits a unique solution. Also, the numerical solver employed for this work is deterministic in that two model runs conducted with perfectly identical setups will produce identical results.…”
Section: Results: Display Of Deterministic Chaosmentioning
confidence: 99%
“…Moreover, for realistic applications, featuring an unsteady flow regime and in‐channel vegetation (e.g., Stecca et al., 2022), the time frame needed for homogeneity is likely to increase even further. In particular, the effects of vegetation are to locally increase roughness, decrease sediment transport, and strengthen banks (Gurnell, 2014), which collectively introduce a localized forcing that increases the degree of inhomogeneity.…”
Section: Discussionmentioning
confidence: 99%
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“…1-100 km). They provide insights on the role of vegetation in modulating alternate bar morphodynamics [11][12][13][14], on the impacts of different root systems [15], on braided morphodynamics [16], and on long-term biogeomorphic succession [17]. They include the effect of vegetation on flow resistance and shear stress, as well as the scouring and deposition processes on vegetation survival and establishment.…”
Section: Motivation and Significancementioning
confidence: 99%