Abstract
By large scale circulation in lakes one means motions whose characteristic length scales extend over most parts or all of the water masses in a lake or the ocean. We present the governing equations and motivate, by means of a scale analysis, the various simplified versions of model equations that are in use in computational lake dynamics. This scale analysis not only permits rational deduction of the reduced equations, it equally provides a means of estimating their limitations. These are discussed as are the difficulties and the peculiarities inherent in the proposed equation sets.
Special features of external and internal wave motions are studied. For barotropic oscillations of a lake system (Lake of Lugano) it is shown that substantial water masses are exchanged between the individual basins at the resonating periods. Baroclinic seiches of a three layer model in which each layer is effective within its own domain show (for the North basin of the Lake of Lugano) that mode structures may differ from layer to layer pointing at important modifications of classical interpretations of higher baroclinic wave dynamics. And in large lakes in the equatorial belt theβ-effect forces modifications of the classical understanding of seiche behavior. Long periodic oscillating features may be attributed to topographic Rossby waves or higher baroclinic internal gravity waves; the observational identification is, however, difficult because lack of spatial resolution of the data makes this identification non-unique. We, finally present results of a full nonlinear numerical baroclinic circulation model and demonstrate that it is able to reproduce the gross features of the immediate response to strong storms during a few days.
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This paper is an extended version of a lecture with the same title, held by K. Hutter on June 14, 1989, at the Workshop “Spatial and temporal scales of water bodies” of the Sonderforschungsbereich “Stoffhaushalt des Bodens”, Universität Konstanz. The character of the paper is that of areview, however, it contains material, theoretical, computational and observational, that has never been presented before to make it sufficiently unique. Some of the new material has been collected and gathered by E. Bäuerle, G. Salvadè, C. Spinedi and F. Zamboni, who should be credited for it, even though none of these people contributed to the layout and drafting of the text, for which K. Hutter is responsible alone.
We thank Professor Max Tilzer of the University Konstanz for inviting K. Hutter to the workshop and giving him the opportunity to present the material as of that time.
As far as referencing current literature is concerned we are neither exhaustive nor complete and only refer to literature which is directly related to the material presented. For a list with more than 300 relevant references, the reader may consult the article “Hydrodynamic Modeling of Lakes” by K. Hutter in the Encyclopedia of Fluid Mechanics, Gulf Publ. Company, Houston Texas (1987). I would like to express my sincere thanks to Mrs. Danner for her diligent work in typing the text.
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Hutter, K., Salvadè, G., Spinedi, C. et al. Large scale water movements in lakes. Aquatic Science 53, 100–135 (1991). https://doi.org/10.1007/BF00877057
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DOI: https://doi.org/10.1007/BF00877057