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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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This paper provides experimental evidence of the occurrence of large and periodic movements induced by the wind at 95 m in depth in Lake Iseo, where a permanent chemocline is located. These movements determine vertical oscillations of the oxycline up to 20 m. Accordingly, in 3 % of the sediment area alternating redox conditions occur, which might force unsteady sediment–water fluxes. This finding has major implications for the internal matter cycle in Lake Iseo.
HESS | Articles | Volume 23, issue 3
Hydrol. Earth Syst. Sci., 23, 1763–1777, 2019
https://doi.org/10.5194/hess-23-1763-2019

Special issue: Modelling lakes in the climate system (GMD/HESS inter-journal...

Hydrol. Earth Syst. Sci., 23, 1763–1777, 2019
https://doi.org/10.5194/hess-23-1763-2019

Research article 02 Apr 2019

Research article | 02 Apr 2019

Oxycline oscillations induced by internal waves in deep Lake Iseo

Giulia Valerio et al.

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Latest update: 20 Jan 2021
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Short summary
This paper provides experimental evidence of the occurrence of large and periodic movements induced by the wind at 95 m in depth in Lake Iseo, where a permanent chemocline is located. These movements determine vertical oscillations of the oxycline up to 20 m. Accordingly, in 3 % of the sediment area alternating redox conditions occur, which might force unsteady sediment–water fluxes. This finding has major implications for the internal matter cycle in Lake Iseo.
Citation