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Research Article

A simple model for predicting oxygen depletion in lakes under climate change

ORCID Icon, ORCID Icon, ORCID Icon & ORCID Icon
Received 04 Jul 2023, Accepted 04 Jan 2024, Published online: 03 May 2024

Figures & data

Table 1. Empirical estimates of VHOD rates obtained from literature for corresponding lakes, years, and trophic status.

Figure 1. Study lakes in Germany (black points) denoting where stratification duration and mean hypolimnion temperature data were observed. Points for Breiter Luzin, Schmaler Luzin, and Feldberger Haussee overlap.

Figure 1. Study lakes in Germany (black points) denoting where stratification duration and mean hypolimnion temperature data were observed. Points for Breiter Luzin, Schmaler Luzin, and Feldberger Haussee overlap.

Table 2. Mean hypolimnion temperature, stratification duration, and model-based VHOD estimates in 13 German lakes.

Figure 2. Mean (black lines) VHOD rates as a function of hypolimnetic temperature for different trophic status. The shaded regions illustrate the 99% confidence interval of each trophic state VHOD mean.

Figure 2. Mean (black lines) VHOD rates as a function of hypolimnetic temperature for different trophic status. The shaded regions illustrate the 99% confidence interval of each trophic state VHOD mean.

Figure 3. Validation of predicted O2 concentrations from our model with in situ measured O2 concentrations from 5 German lakes (Arendsee, Feldberger Haussee, and Tegler See are eutrophic; Breiter Lutzin and Groß Glienicker See are mesotrophic). The regression line (red) is shown with 95% confidence interval (shaded grey area). Blue and dotted line indicates the 1:1 line.

Figure 3. Validation of predicted O2 concentrations from our model with in situ measured O2 concentrations from 5 German lakes (Arendsee, Feldberger Haussee, and Tegler See are eutrophic; Breiter Lutzin and Groß Glienicker See are mesotrophic). The regression line (red) is shown with 95% confidence interval (shaded grey area). Blue and dotted line indicates the 1:1 line.

Figure 4. Contour plots displaying the predicted O2 concentration (color scale) in (a) oligotrophic, (b) mesotrophic, and (c) eutrophic lakes as a function of stratification and hypolimnion temperature. Points denote separate years in a respective lake. Isolines represent O2 concentrations.

Figure 4. Contour plots displaying the predicted O2 concentration (color scale) in (a) oligotrophic, (b) mesotrophic, and (c) eutrophic lakes as a function of stratification and hypolimnion temperature. Points denote separate years in a respective lake. Isolines represent O2 concentrations.

Figure 5. Stratification duration for a lake of a specific trophic state at a given hypolimnetic temperature to reach critical O2 biological and ecological thresholds; anoxia = 0.5 mg L−1 (solid line), hypoxia = 2 mg L−1 (long dash), uninhabitable by cold dwelling fish species = 5 mg L−1 (dot dash). Our reference temperature of 4°C is denoted by the black dotted line.

Figure 5. Stratification duration for a lake of a specific trophic state at a given hypolimnetic temperature to reach critical O2 biological and ecological thresholds; anoxia = 0.5 mg L−1 (solid line), hypoxia = 2 mg L−1 (long dash), uninhabitable by cold dwelling fish species = 5 mg L−1 (dot dash). Our reference temperature of 4°C is denoted by the black dotted line.
Supplemental material

Supplementary Table 1.docx

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Supplementary Table 4.docx

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