Bridging the gap between terrestrial, riverine and limnological research: application of a model chain to a mesotrophic lake in North America
Crossman, J.; Elliott, J.A.. 2018 Bridging the gap between terrestrial, riverine and limnological research: application of a model chain to a mesotrophic lake in North America. Science of the Total Environment, 622-623. 1363-1378. 10.1016/j.scitotenv.2017.12.052
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Abstract/Summary
Models remain our best available tool for managing low lake dissolved oxygen concentrations, which pose a serious ecological risk. This study investigated whether process-based catchment models (INCA-N and INCA-P) could accurately drive a lake model (PROTECH), to bridge a gap between terrestrial, riverine and limnological research. INCA was calibrated over all 20 catchments of the Simcoe watershed, Canada. Daily outputs (flow, nitrogen and phosphorus concentrations) over the period 2010–2016 were selected for a common “baseline” period, and used as inputs to PROTECH, which was calibrated across the three major basins of lake Simcoe; Kempenfelt (K42), Cooks (C9), and the main basin (E51). Results showed that at catchment outflows INCA models achieved an average flow R2 of 0.8; a load R2 of 0.7 (both for TP and N-NO3), a concentration R2 of 0.4 and 0.5 (for TP and N-NO3 respectively), and an SiO2 R2 > 0.8. In each basin PROTECH achieved an R2 for both temperature and dissolved oxygen (DO) concentrations of > 0.9. Performance of N-NO3, TP and Chlorophyll-a concentrations were good (R2 values of up to 0.98, 0.92 and 0.53 respectively). Multi-stressor analyses established that most occurrences when DO dropped below the desired 7 mg/l threshold (DO7) were attributable to combinations of high temperatures and low tributary inflows. The importance of additional drivers was depth dependent, with photosynthesis being particularly important in shallower C9 and E51 basins during summer, when algae contributed sufficient O2 to the water column to inhibit DO7 events. Conversely in the deeper more strongly stratified K42 basin, greater algal growth boosted the biochemical oxygen demand, enhancing declines in DO. Lake physics explained a significant number of DO7 events in all three basins. Integrated catchment-lake modelling approaches are important in understanding lake physical and ecological processes, and the impacts of land management and future climate change.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1016/j.scitotenv.2017.12.052 |
UKCEH and CEH Sections/Science Areas: | Water Resources (Science Area 2017-) |
ISSN: | 0048-9697 |
Additional Information. Not used in RCUK Gateway to Research.: | Open Access paper - full text available via Official URL link. |
Additional Keywords: | dissolved oxygen, chlorophyll-a, phosphorus, flow, temperature, biochemical oxygen demand |
NORA Subject Terms: | Ecology and Environment |
Date made live: | 21 Dec 2017 16:03 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/518810 |
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