Abstract
The dynamics of lakes has a hydrodynamic and a thermodynamic component. By neglection of the latter, assuming a thermally homogeneous water body, a barotropic model is obtained. It is characterized by vanishing horizontal density gradients; the surface slope alone determines the horizontal pressure gradients (H1, section 1)*). Vertical density gradients can be considered by a barotropic multi-layer model (H1, section 5).
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© 1984 Springer-Verlag Wien
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Sündermann, J. (1984). Numerical Modelling of Barotropic Circulation Processes. In: Hutter, K. (eds) Hydrodynamics of Lakes. International Centre for Mechanical Sciences, vol 286. Springer, Vienna. https://doi.org/10.1007/978-3-7091-2634-9_6
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DOI: https://doi.org/10.1007/978-3-7091-2634-9_6
Publisher Name: Springer, Vienna
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