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Updated: Aug 25, 2025

Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
Published on: January 7, 2019
Modelling Subarctic watershed dissolved organic carbon response to hydroclimatic regime
S Sharma1, M N Futter2, C Spence3
1School of Environment and Sustainability, University of Saskatchewan, Saskatoon, SK S7N 3H5, Canada; Global Institute for Water Security, University of Saskatchewan, Saskatoon, SK S7N 3H5, Canada.
Climate change impacts northern watersheds. Warmer, wetter conditions may increase carbon export by up to 81%, especially in early winter, necessitating further monitoring of these vital ecosystems.
Area of Science:
- Environmental science
- Hydrology
- Climate change research
Background:
- Global climate change is altering hydroclimatic regimes, affecting freshwater resources.
- Northern hemisphere high latitudes store significant terrestrial carbon, making them vulnerable to changing water patterns.
- Understanding carbon budgets and pollutant transfer is crucial for assessing climate change impacts in these regions.
Purpose of the Study:
- To model streamflow, dissolved organic carbon (DOC) concentration, and DOC export in a warming northern Canadian catchment.
- To project the effects of future climate scenarios on carbon dynamics.
- To inform strategies for monitoring and managing northern freshwater ecosystems.
Main Methods:
- Utilized a dynamic modeling approach with the Integrated Catchment model for Carbon (INCA-C).
- Calibrated the model using multi-year data (2012-2016) representing diverse hydrologic conditions.
- Simulated model runs over 30-year periods for baseline and two future climate scenarios (elevated temperature, and elevated temperature with precipitation).
Main Results:
- Predicted decreased average discharge (22-27%) under elevated temperature, but increased discharge (116-175%) under elevated temperature and precipitation.
- Projected a shift from a nival to a combined nival and pluvial hydroclimatic regime under the warmer, wetter scenario.
- Anticipated a decrease in average DOC flux (24-27%) with elevated temperature alone, but a significant increase (64-81%) under elevated temperature and precipitation due to enhanced catchment connectivity.
- Identified early winter as the period with the largest projected increase in DOC export.
Conclusions:
- Future climate scenarios, particularly warmer and wetter conditions, are predicted to significantly increase carbon export from northern catchments.
- Changes in dissolved organic carbon export suggest potential for broader ecosystem shifts.
- Increased carbon export, especially in early winter, highlights the need for enhanced monitoring in vulnerable northern regions.
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