4.7 Article

Catchment Functioning Under Prolonged Drought Stress: Tracer-Aided Ecohydrological Modeling in an Intensively Managed Agricultural Catchment

Journal

WATER RESOURCES RESEARCH
Volume 57, Issue 3, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020WR029094

Keywords

drought stress; ecohydrological functioning; multi‐ criteria calibration; stable isotopes of water and water ages; tile drainage; tracer‐ aided modeling

Funding

  1. Terrestrial Environmental Observatories (TERENO) project under the Earth and Environment Program of the Helmholtz Association, Germany
  2. Modular Observation Solutions for Earth Systems (MOSES) project, under the Earth and Environment Program of the Helmholtz Association, Germany
  3. Leverhulme Trust's ISOLAND project

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The research reveals that high spatial heterogeneity in catchment properties can amplify ecohydrological responses to changing conditions, as demonstrated by investigating a small agricultural catchment in central Germany during drought using a tracer-aided model. Environmental data collected during drought years were found to be highly informative in modeling stream water dynamics, and inclusion of isotope data helped reduce model uncertainty and improve confidence in simulations. The study highlights the importance of understanding the variability of internal ecohydrological processes and the different responses of fluxes and water ages to prolonged drought stress in agricultural headwater ecosystems.
High spatial heterogeneity of catchment properties enhances the variability of ecohydrological responses to changing natural and anthropogenic conditions, like the European-wide droughts in 2018-2019. Based on new adaptations of a tracer-aided, process-based ecohydrological model (EcH(2)O-iso), we investigated drought-induced nonstationary ecohydrological behavior in a small agricultural headwater catchment (1.44 km(2)) in central Germany. Multiple environmental time-series helped inform various aspects of catchment functioning that have been impacted by agricultural activity and changing climate conditions and helped to further constrain model calibration. Multi-criteria calibration showed that data collected during drought years were highly informative in reproducing the changes in stream water dynamics. Further, inclusion of delta 2H and delta 18O data was valuable for reducing model uncertainty and increasing confidence in simulations of green- and blue-water flux partitioning and storage-flux-age interactions. Using the best-performing calibrations, we further analyzed the high spatiotemporal variability of internal ecohydrological processes and the varying responses of fluxes and associated water ages to prolonged drought stress. Under drought conditions, modeled stream runoff contributed from deeper, older storages increased significantly after a particularly wet season, resulting in a sharp increase in stream water age. Unlike relatively minor changes in soil evaporation, seasonally typical transpiration fluxes were initially maintained in April-June but dramatically decreased as the drought further developed in July-September. Importantly, the tracer-based transpired water age was much older after April, providing a potential indicator of drought impacts and the need for precautionary management responses. Our findings are important for similar agricultural headwater ecosystems in other drought-sensitive regions.

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