Mixing processes in lakes: mechanisms and ecological relevance View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1983-03

AUTHORS

D. M. Imboden, U. Lemmin, T. Joller, M. Schurter

ABSTRACT

In Lake Baldegg, Switzerland (surface area 5.3 km2, maximum depth 66 m) the analysis of data from moored instrument systems (atmospheric boundary layer, lake temperature distribution, bottom currents) was correlated to the long-term development of vertical mixing as seen from profiles of natural isotopes (radon-222, tritium and helium-3) and chemical species. The investigation shows: 1. Vertical mixing coefficients below 25 m are small. Consequently the vertical concentration distribution of sediment emanating species in the deep hypolimnion is controlled by the bottom topography. 2. Renewal of deep hypolimnic water is significant even during stratification. 3. Weakly damped internal waves characterize the internal dynamics during stratification. 4. Horizontal bottom currents play an important role in the hypolimnion mixing and can be correlated to internal waves during stratification. More... »

PAGES

11-44

References to SciGraph publications

  • 1953-06. The resonant response of stratified lakes to wind in SWISS JOURNAL OF HYDROLOGY
  • 1973-03. Vertical eddy diffusion coefficient in Lake Zürich in SWISS JOURNAL OF HYDROLOGY
  • 1973-03. Limnologische Transport- und Nährstoffmodelle in SWISS JOURNAL OF HYDROLOGY
  • 1972-03. An approach to the modeling of lakes in SWISS JOURNAL OF HYDROLOGY
  • 1979-09. MELIMEX, an experimental heavy metal pollution study: Vertical mixing in a large limno-corral in SWISS JOURNAL OF HYDROLOGY
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    http://scigraph.springernature.com/pub.10.1007/bf02538150

    DOI

    http://dx.doi.org/10.1007/bf02538150

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