Preprints
https://doi.org/10.5194/egusphere-2026-303
https://doi.org/10.5194/egusphere-2026-303
02 Feb 2026
 | 02 Feb 2026
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Causal drivers of alpine flood variability from 1300 to 2020 revealed by climate time series analysis

Juan Carlos Peña-Rabadán, Lothar Schulte, Josep Ramon Miró-Cubells, Enric Casellas-Masana, and Filipe Carvalho

Abstract. Understanding flood variability in the European Alps is critical for risk management, yet causal mechanisms linking climate drivers to floods remain unclear. Previous studies have largely relied on correlations, limiting causal attribution. Here we apply a constraint-based causal inference framework using the PC-stable algorithm, combined with bootstrap stability analysis and Granger causality validation, to multi-centennial climate and flood proxy records from the Hasli-Aare catchment (1300–2020 CE). Our results reveal that total solar irradiance modulates summer atmospheric circulation, notably the summer North Atlantic Oscillation, which causally influences alpine flood frequency. These relationships are strongest during the preindustrial period and weaken under modern anthropogenic forcing, indicating a shift in dominant flood drivers. Our study demonstrates the utility of causal inference methods in paleoclimate research and offers a framework for investigating changes in the drivers of hydrological extremes, important for climate attribution and risk assessment in mountain environments.

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Juan Carlos Peña-Rabadán, Lothar Schulte, Josep Ramon Miró-Cubells, Enric Casellas-Masana, and Filipe Carvalho

Status: open (until 16 Mar 2026)

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Juan Carlos Peña-Rabadán, Lothar Schulte, Josep Ramon Miró-Cubells, Enric Casellas-Masana, and Filipe Carvalho
Juan Carlos Peña-Rabadán, Lothar Schulte, Josep Ramon Miró-Cubells, Enric Casellas-Masana, and Filipe Carvalho
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Latest update: 03 Feb 2026
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Short summary
1. Total Solar Irradiance is a key external driver modulating summer atmospheric modes, which in turn influence alpine flood frequency. 2. These causal pathways are strongest in preindustrial era, suggesting enhanced solar-atmospheric coupling in the absence of strong anthropogenic forcing. 3. The causal structure is statistically stable and physically consistent, validated across methods and time periods.
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