Merz et al. (2026) Disentangling the anthropogenic climate change influence on recent hydroclimate whiplash events via multiple nudged model simulations
Identification
- Journal: npj Climate and Atmospheric Science
- Year: 2026
- Date: 2026-10-28
- Authors: Niklas Merz, Jakob Zscheischler A, István Dunkl, Sebastian Sippel, Antonio Sánchez-Benítez, Helge Goessling, Amal John, Frauke Feser, Emanuele Bevacqua
- DOI: 10.1038/s41612-026-01578-3
Research Groups
- Department of Compound Environmental Risks, Helmholtz Centre for Environmental Research - UFZ, Leipzig, Germany
- Department of Hydro Sciences, TUD Dresden University of Technology, Dresden, Germany
- Institute for Meteorology, Leipzig University, Leipzig, Germany
- Alfred Wegener Institute, Helmholtz-Centre for Polar and Marine Research, Bremerhaven, Germany
- Institute of Coastal Systems, Helmholtz-Zentrum Hereon, Geesthacht, Germany
Short Summary
This study quantifies the anthropogenic climate change influence on the intensity of nine recent hydroclimate whiplash events using a multi-model ensemble of wind-nudged simulations, revealing that climate change accounts for an average of 9% of observed whiplash intensity, primarily driven by non-linear increases in potential evapotranspiration.
Objective
- To quantify thermodynamically-driven changes in hydroclimate whiplash intensity for nine high-impact events using the Standardised Precipitation Evapotranspiration Index (SPEI) and a multi-model ensemble of wind-nudged storyline simulations.
- To disentangle the anthropogenic contributions to whiplash intensity arising from changes in precipitation and potential evapotranspiration.
Study Configuration
- Spatial Scale: Nine high-impact regional events across the globe, analyzed on a 0.5° × 0.5° grid.
- Temporal Scale: Recent decade (events from the past decade, e.g., 2017–2024 for event periods); SPEI-3 (3-month moving average) and SPEI-12 (12-month moving average) timescales; calibration periods from 1980–2024 or 1980–2014.
Methodology and Data
- Models used: CESM2, IFS-FESOM, AWI-CM-1, ECHAM6 (all circulation-nudged climate models).
- Data sources: ERA5 global reanalysis dataset (1940–2024), NCEP-NCAR Reanalysis 1 (for ECHAM6 nudging).
Main Results
- Anthropogenic climate change accounts for an average of 9% (range across events: -2% to 72%) of the observed whiplash intensity, with positive contributions for nearly all events according to the multi-model mean.
- This climate change contribution is predominantly driven by a non-linear increase in potential evapotranspiration (PET), which strengthens drying more during the dry phase (mean 12% contribution) than during the wet phase (mean -7% contribution).
- Precipitation changes contribute a smaller and less robust mean signal of 4%.
- Models agree on the positive climate change contribution for six of the nine events (approximately two-thirds).
- Model uncertainty on the magnitude of the climate change contribution is substantial, with an average inter-model spread of 13% across events (9%/°C when normalized by warming level).
- Events in regions dominated by organized deep convection or complex ocean-land interactions (e.g., West Africa, East Africa, Central America) proved most difficult for the nudged simulations to reproduce.
Contributions
- Provides the first quantification of the anthropogenic contribution to the intensity of specific, historically observed hydroclimate whiplash events, complementing previous studies focused on long-term changes in frequency or intensity of generic events.
- Utilizes a unique multi-model ensemble of wind-nudged storyline simulations, which constrains large-scale atmospheric circulation to observations, thereby isolating thermodynamic responses to anthropogenic warming and reducing uncertainty from free-running models.
- Disentangles the contributions of precipitation and potential evapotranspiration, revealing that the asymmetric enhancement of PET (stronger drying during dry phases) is the primary driver of whiplash intensification.
- Highlights the critical importance of employing multiple independently developed nudged datasets to enhance robustness and adequately capture structural uncertainty in event-based attribution analyses of complex events.
Funding
- Program-oriented funding of the Helmholtz Association
- Helmholtz Centre for Environmental Research SEESAW PhD cohort
- German Federal Environmental Foundation (DBU) (AZ: 20025/114)
- Deutsche Forschungsgemeinschaft (DFG) Emmy Noether Programme (grant ID 524780515)
- SMWK (Sächsisches Staatsministerium für Wissenschaft, Kultur und Tourismus) [3-7304/44/4-2023/8846] (Breathing Nature initiative)
- EU Horizon project ‘Artificial Intelligence for Enhanced Representation of Processes and Extremes in Earth System Models’ (AI4PEX; grant agreement 101137682)
- Helmholtz Research Field Earth & Environment for the Innovation Pool Project Actuate
- BMFTR-projects ClimXtreme-A5 (01 LP 2322 B) and WAKOS-2 (01LR2003A1)
- Helmholtz Climate Initiative (HICAM)—Phase 2
- European Union’s ‘Destination Earth’ initiative
Citation
@article{Merz2026Disentangling,
author = {Merz, Niklas and A, Jakob Zscheischler and Dunkl, István and Sippel, Sebastian and Sánchez-Benítez, Antonio and Goessling, Helge and John, Amal and Feser, Frauke and Bevacqua, Emanuele},
title = {Disentangling the anthropogenic climate change influence on recent hydroclimate whiplash events via multiple nudged model simulations},
journal = {npj Climate and Atmospheric Science},
year = {2026},
doi = {10.1038/s41612-026-01578-3},
url = {https://doi.org/10.1038/s41612-026-01578-3}
}
Original Source: https://doi.org/10.1038/s41612-026-01578-3