Preprints
https://doi.org/10.5194/egusphere-2025-6372
https://doi.org/10.5194/egusphere-2025-6372
30 Dec 2025
 | 30 Dec 2025
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Climate and landscape jointly control Europe's hydrology

Julia M. Rudlang, Thiago V. M. do Nascimento, Ruud van der Ent, Fabrizio Fenicia, and Markus Hrachowitz

Abstract. The complex composition of hydrological systems, climates and landscapes makes it challenging to explain and predict hydrological streamflow response. Many previous large-sample studies, mostly focused on the United States, identified climate as the primary control, with landscape exerting only a minor role in shaping hydrological behaviour. Yet, a few other studies report contradicting results with landscape being a more dominant driver. In this study, we use an unprecedentedly large sample of more than 7000 catchments in Europe from the EStreams dataset to identify and map functionally similar catchments, together with their spatially variable climate and landscape controls. The wide spatial and temporal gradient of the study catchments was used to identify hydrological response types (HRTs) based on 40 hydrological streamflow signatures related to long-term averages and inter-annual variability of magnitude, timing, duration, frequency, and seasonality. Overall, 10 HRTs could be identified. Several HRTs are well defined and well distinguishable, largely due to catchments with strongly seasonal or more extreme behaviour. Other HRTs remain difficult to distinguish, as these catchments represent more transitional conditions with increasingly overlapping characteristics between HRTs. The underlying drivers of the HRTs were identified by using 84 climate- and landscape attributes to predict catchment membership to their respective HRT with a Random Forest classification model. Climate emerges as the dominant driver of hydrological behaviour at the continental scale. However, landscape was found, in 4 out of 10 HRTs, to be at least as strong or even stronger a control on the hydrological response. These results highlight that the complex, integrated nature of hydrological response remains challenging to disentangle, even with extensive datasets and advanced modelling approaches, and therefore, climate and landscape needs to be understood as joint drivers in a co-evolutionary perspective.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Hydrology and Earth System Sciences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Julia M. Rudlang, Thiago V. M. do Nascimento, Ruud van der Ent, Fabrizio Fenicia, and Markus Hrachowitz

Status: open (until 10 Feb 2026)

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Julia M. Rudlang, Thiago V. M. do Nascimento, Ruud van der Ent, Fabrizio Fenicia, and Markus Hrachowitz

Data sets

EStreams: An Integrated Dataset and Catalogue of Streamflow, Hydro-Climatic Variables and Landscape Descriptors for Europe (1.2) Thiago V. M. do Nascimento et al. https://doi.org/10.5281/zenodo.14778580

Model code and software

Code used in: Climate and landscape jointly control Europe's hydrology Julia M. Rudlang https://doi.org/10.5281/zenodo.17987885

Julia M. Rudlang, Thiago V. M. do Nascimento, Ruud van der Ent, Fabrizio Fenicia, and Markus Hrachowitz
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Latest update: 30 Dec 2025
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Short summary
River flow behaviour varies across Europe and is shaped by both climate and landscape. Using streamflow data from more than 7000 European catchments, we identified 10 distinct hydrological response types based on flow magnitude, timing, and seasonality. Climate is the main control at the continental scale, but landscape features are equally important or more influential in several regions. These results show that river behaviour emerges from the combined effects of climate and landscape.
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