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| Created: | Mar 12, 2025 at 9:55 p.m. (UTC) | |
| Last updated: | Feb 06, 2026 at 12:13 p.m. (UTC) | |
| Citation: | See how to cite this resource |
| Sharing Status: | Private (Accessible via direct link sharing) |
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| Views: | 33 |
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Abstract
Hydrometeorological drivers, including biogeochemical processes, water availability, and soil properties, influence dissolved organic carbon (DOC) fluxes in catchments. We developed a simple, parsimonious model to examine these factors and calibrated it to simulate discharge and DOC dynamics simultaneously. The model was applied to a temperate, wetland-dominated catchment using over 14 years of high-resolution hydrological data and DOC concentration measurements taken weekly to monthly intervals across nested catchments (7 km², 170 km², and 480 km²). The simulations effectively captured daily hydrological and DOC concentration dynamics across all catchments, achieving a Kling-Gupta Efficiency (KGE) of approximately 0.60. Full results and interpretations are detailed in the paper published at EEEEEEEEEE. To support reproducibility, we have organized all input and output data into accessible resources.
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Related Resources
| Title | Owners | Sharing Status | My Permission |
|---|---|---|---|
| DOC-Model resources: Optimization of parsimonious and synchronized discharge and dissolved organic carbon models across scales | Gabriel V. Gaona Gaona · Juan Pesantez | Private & Shareable | None |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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