Preprints
https://doi.org/10.5194/egusphere-2025-3255
https://doi.org/10.5194/egusphere-2025-3255
05 Aug 2025
 | 05 Aug 2025
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Simulating carbon fluxes in boreal catchments: WSFS-Vemala model development and key insights

Marie Korppoo, Inese Huttunen, Markus Huttunen, Maiju Narikka, Jari Silander, Tom Jilbert, Martin Forsius, Pirkko Kortelainen, Niina Kotamäki, Cintia Uvo, and Anna-Kaisa Ronkanen

Abstract. Lakes and streams play an important role in the global carbon cycle through carbon sedimentation and evasion. The development of carbon processes in the water quality model WSFS-Vemala (Vemala) presents a significant advancement in simulating carbon dynamics, particularly in capturing both total organic (TOC) and inorganic (TIC) carbon processes and their contributions to carbon retention and emissions through a river/lake network. The model was tested in the Vantaanjoki catchment, located in southern Finland and covering an area of 1680 km2. The model's ability to simulate TOC and TIC loading across various land use and soil types aligns closely with reported literature values. The addition of organic acids to the total alkalinity definition improved pH simulations and thus the simulation of CO2 emissions in the acidic and organic rich waters of Finland. Annual CO2 emissions of 25 gC m2 yr-1 were simulated from lake Tuusulanjärvi, the largest lake in the catchment, and 223–260 gC m-2 yr-1 from the river network, while only 3 gC m-2 yr-1 was simulated as organic carbon burial in the lake sediments. The model's performance in estimating CO2 emissions shows good correlations with established ranges for lakes as well as good correlation with TOC and TIC loads across the river network. The inclusion of sedimentation and mineralization processes in the lake carbon budget underlines the necessity of accounting for both organic and inorganic pathways in carbon modelling. This improved representation of the carbon cycling in Vemala, linked with the phytoplankton growth and nutrient cycling, allow to distinguish between carbon losses to the atmosphere and long-term carbon storage in the sediments of inland waters. Overall, the enhanced Vemala model provides a robust foundation for understanding carbon cycling and supporting sustainable, integrated water resource management and scenario assessments from sub-catchments to the national scale.

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Marie Korppoo, Inese Huttunen, Markus Huttunen, Maiju Narikka, Jari Silander, Tom Jilbert, Martin Forsius, Pirkko Kortelainen, Niina Kotamäki, Cintia Uvo, and Anna-Kaisa Ronkanen

Status: open (until 23 Oct 2025)

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Marie Korppoo, Inese Huttunen, Markus Huttunen, Maiju Narikka, Jari Silander, Tom Jilbert, Martin Forsius, Pirkko Kortelainen, Niina Kotamäki, Cintia Uvo, and Anna-Kaisa Ronkanen
Marie Korppoo, Inese Huttunen, Markus Huttunen, Maiju Narikka, Jari Silander, Tom Jilbert, Martin Forsius, Pirkko Kortelainen, Niina Kotamäki, Cintia Uvo, and Anna-Kaisa Ronkanen

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Short summary
The development of carbon processes in the water quality model WSFS-Vemala presents a significant advancement in simulating both total organic and inorganic carbon dynamics, burial and emissions through a river/lake network. The addition of organic acids to the total alkalinity definition improved pH simulations and thus the simulation of CO2 emissions in the acidic and organic rich waters of Finland. The new Vemala model provides a robust foundation to support water management in the future.
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