pydune.physics.dune.bedinstability_2D#
Dune flat bed instability taking into account two spatial direction (x and y), under unidirectional, bidirectional and multidirectional wind regimes. Here, only the temporal instability is derived, following Gadal et al. 2019.
where \(Q_{*}\) is a characteristic sand flux, \(\omega\) a dimensional constant, \(u_{*}\) the wind shear velocity and u_{rm th} the threshold velocity for sediment transport.
In the following, all quantities are made non-dimensional:
length scales by the saturation length \(L_{\rm sat}\).
time scales by \(L_{\rm sat}^{2}/Q_{*}\).
References
Functions
Celerity \(\sigma\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by a bidirectional wind whose orientation alternates regularly between \(-\theta/2\) and \(+\theta/2\). |
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Cosine element-wise |
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Temporal growth rate \(\sigma\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by a bidirectional wind whose orientation alternates regularly between \(-\theta/2\) and \(+\theta/2\). |
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Trigonometric sine using |
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Temporal celerity \(c = \omega/k\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by a unidirectional constant wind through the linear dune instability. |
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Temporal celerity \(c\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by succesion of winds of various orientations and strengths. |
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Temporal growth rate of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by a unidirectional constant wind through the linear dune instability. |
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Temporal growth rate \(\sigma\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by succesion of winds of various orientations and strengths. |
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Temporal pulsation \(\omega\) of sinusoidal periodic dunes of wavenumber \(k\) and orientation \(\alpha\) induced by a unidirectional constant wind through the linear dune instability. |