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DOC-hydro model: inputs and outputs


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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)
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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.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Lamprey River Hydrologic Observatory
North Latitude
43.2313°
East Longitude
-70.7684°
South Latitude
42.9746°
West Longitude
-71.3686°

Temporal

Start Date:
End Date:

Content

Related Resources

This resource belongs to the following collections:
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

Pesantez, J., C. Birkel, G. V. Gaona Gaona, W. H. McDowell, M. Shattuck, J. Potter, A. Contosta, A. Wymore (2026). DOC-hydro model: inputs and outputs, HydroShare, http://www.hydroshare.org/resource/8159b32b070e4075a137ae3a44f3f9c8

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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