Can linear stability analyses predict the development of river bed waves
with lengths much larger than the water depth?
Abstract
Sustainable river management can be supported by models predicting
long-term morphological developments. Even for one-dimensional
morphological models, run times can be up to several days for
simulations over multiple decades. Alternatively, analytical tools yield
metrics that allow estimation of migration celerity and damping of bed
waves, which have potential for being used as rapid assessment tools to
explore future morphological developments. We evaluate the use of
analytical relations based on linear stability analyses of the St.
Venant-Exner equations, which apply to bed waves with spatial scales
much larger than the water depth. With a one-dimensional numerical
morphological model, we assess the validity range of the analytical
approach. The comparison shows that the propagation of small bed
perturbations is well-described by the analytical approach. For Froude
numbers over 0.3, diffusion becomes important and bed perturbation
celerities reduce in time. A spatial-mode linear stability analysis
predicts an upper limit for the bed perturbation celerity. For longer
and higher bed perturbations, the dimensions relative to the water depth
and the backwater curve length determine whether the analytical approach
yields realistic results. For higher bed wave amplitudes, non-linearity
becomes important. For Froude numbers ≤0.3, the celerity of bed waves is
increasingly underestimated by the analytical approach. The degree of
underestimation is proportional to the ratio of bed wave amplitude to
water depth and the Froude number. For Froude numbers exceeding 0.3, the
net impact on the celerity depends on the balance between the decrease
due to damping and the increase due to non-linear interaction.