Titlebook: Hydrodynamics of Lakes; K. Hutter Book 1984 Springer-Verlag Wien 1984 Hydrodynamik.See.dynamics.hydrodynamics

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Hydrodynamics of Lakes978-3-7091-2634-9Series ISSN 0254-1971 Series E-ISSN 2309-3706

Lyme-disease

0254-1971 Overview: 978-3-211-81812-1978-3-7091-2634-9Series ISSN 0254-1971 Series E-ISSN 2309-3706

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Numerical Modelling of Barotropic Circulation Processes,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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https://doi.org/10.1007/978-3-7091-2634-9Hydrodynamik; See; dynamics; hydrodynamics

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Some Aspects of Baroclinic Circulation Models,ion of a lake” and may mean by it the average of several years of stratified circulation patterns in summer. However, even the response of a lake to a few days of wind forcing is often referred to as “circulation”; in this case it means that also wave processes of this time scale have to be included.

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Topographic Waves in Lakes,nd quasi-geostrophic waves) was given by Lamb (1932). However, it is only very recently (e.g., see Saylor et al., 1980) that observations and an appropriate theory have been combined to provide a unified account of low-frequency motions in lakes.