The DOI matches its Crossref record; 62 of the 62 references it cites were found in a registry or an index.
S MALL-S CALE H YDRODYNAMICS IN L AKES
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▪ Abstract Recent small-scale turbulence observations allow the mixing regimes in lakes, reservoirs, and other enclosed basins to be categorized into the turbulent surface and bottom boundary layers as well as the comparably quiet interior. The surface layer consists of an energetic wave-affected thin zone at the very top and a law-of-the-wall layer right below, where the classical logarithmic-layer characteristic applies on average. Short-term current and dissipation profiles, however, deviate strongly from any steady state. In contrast, the quasi-steady bottom boundary layer behaves almost perfectly as a logarithmic layer, although periodic seiching modifies the structure in the details. The interior stratified turbulence is extremely weak, even though much of the mechanical energy is contained in baroclinic basin-scale seiching and Kelvin waves or inertial currents (large lakes). The transformation of large-scale motions to turbulence occurs mainly in the bottom boundary and not in the interior, where the local shear remains weak and the Richardson numbers are generally large.
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Stockwell, J. D., Doubek, J. P., Adrian, R., Anneville, O., Carey, C. C., Carvalho, L., De Senerpont Domis, L. N., Dur, G., Frassl, M. A., Grossart, H., et al. (2020) · Global Change Biology · doi:10.1111/gcb.15033 · Cited by 293
Wind sheltering of a lake by a tree canopy or bluff topography
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Metadata
- Authors
- Wüest, A., & Lorke, A.
- Venue
- Annual Review of Fluid Mechanics
- Publisher
- Annual Reviews
- Published
- 2003-01
- Volume
- 35
- Issue
- 1
- Pages
- 373-412
- ISSN
- 0066-4189 (ISSN-L)
- 1545-4479
- OpenAlex
- W2126080245
- Cited by
- 592
- References
- 62
- FWCI
- 4.81
- Type
- journal article
- Language
- en
- Open access
- green
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