Abstract.
Vertical transport in a small eutrophic lake was investigated. The study site is a gravel pit lake in the Upper Rhine Graben near Ludwigshafen, Germany (800 × 250 m, mean depth 9 m, maximum depth 20 m). The governing mixing processes show patterns influenced by a strong density stratification. From weekly measured temperature profiles, we quantitatively estimated profiles of effective vertical transport coefficients K z . In the stratified regions, K z is at the level of heat conduction (~1.4·10-7 m2/s). Towards the lake bottom, we found a characteristic increase of K z to values up to 10−5 m2/s. Using a bottom-mounted 1,200 kHz-ADCP, we performed velocity measurements with a high vertical and temporal resolution (0.2 to 0.4 m and 5 min, respectively) of the horizontal currents. Using these horizontal flow data and stability profiles, Richardson numbers were analysed for a period of 5 weeks during summer stratification. The simultaneous measurements of currents and vertical diffusion coefficients allowed us to check a given parameterisation of K z (Ri) and to discuss its applicability to the investigated system.
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Received: 16 September 2005; revised manuscript accepted: 28 August 2006
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von Rohden, C., Wunderle, K. & Ilmberger, J. Parameterisation of the vertical transport in a small thermally stratified lake. Aquat. Sci. 69, 129–137 (2007). https://doi.org/10.1007/s00027-006-0827-4
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DOI: https://doi.org/10.1007/s00027-006-0827-4