Holtanová et al. (2025) Scenarios of Köppen-Trewartha climate types in Europe based on GCM-RCM combined projections
Identification
- Journal: Theoretical and Applied Climatology
- Year: 2025
- Date: 2025-10-18
- Authors: Eva Holtanová, Michal Belda, Herijaona Hani‐Roge Hundilida Randriatsara, Amanda Imola Szabó, Tomáš Halenka
- DOI: 10.1007/s00704-025-05806-3
Research Groups
- Department of Atmospheric Physics, Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic
Short Summary
This study assesses projected changes in Köppen-Trewartha climate types across Europe throughout the 21st century using a novel hybrid method that combines global and regional climate model outputs. It finds a significant northward and eastward shift of climate zones, with colder types shrinking and warmer, drier types expanding, particularly in southern Europe, providing an updated CMIP6-based assessment.
Objective
- To assess projected changes in the distribution of Köppen-Trewartha climate types over Europe throughout the 21st century under two socio-economic scenarios.
- To investigate the boundary shifts between Europe’s most common climate types (temperate D and boreal E).
- To evaluate the utility of a hybrid method combining Global Climate Model (GCM) and Regional Climate Model (RCM) outputs for climate change assessment, incorporating the full GCM ensemble.
Study Configuration
- Spatial Scale: Europe, with data remapped to a 0.1° latitude/longitude horizontal resolution (approximately 11 km at mid-latitudes) for observational data and 110 meters (0.11 km) for RCM simulations.
- Temporal Scale: Reference period 1971–2000, and six 30-year future periods: 2016–2045, 2026–2055, 2036–2065, 2046–2075, 2056–2085, and 2066–2095.
Methodology and Data
- Models used:
- Köppen-Trewartha Classification (KTC) scheme.
- Hybrid method (Ruosteenoja and Räisänen, 2024) to combine GCM and RCM outputs, using multiplicative form for temperature changes and summation form for precipitation changes.
- Delta approach (change-factor method) for bias adjustment of temperature and precipitation projections.
- Data sources:
- Observational data: E-OBS dataset version 30.0e (0.1° horizontal resolution).
- Global Climate Models (GCMs): Multi-model ensembles from CMIP5 and CMIP6.
- Regional Climate Models (RCMs): Multi-model ensemble from EURO-CORDEX (0.11 km horizontal resolution).
- Socio-economic scenarios: Representative Concentration Pathways (RCP4.5, RCP8.5) for CMIP5/EURO-CORDEX and Shared Socioeconomic Pathways (SSP2-4.5, SSP5-8.5) for CMIP6.
Main Results
- Colder climate types (tundra Ft, continental boreal Ec, oceanic boreal Eo, continental temperate Dc) are projected to shrink and shift northward and/or eastward across Europe.
- Warmer and drier climate types (oceanic temperate Do, humid subtropical Cf, steppe BS, Mediterranean Cs) are expected to expand.
- The continental boreal Ec type and tundra Ft type are projected to shrink radically, with Ec practically disappearing by the end of the 21st century under SSP2-4.5 and by mid-century under SSP5-8.5.
- Oceanic boreal Eo is projected to shrink from 12% (2016–2045) to 3% (SSP5-8.5) or 9% (SSP2-4.5) of the European domain by the end of the century (hybrid-CMIP6).
- The oceanic temperate Do type is projected for the largest expansion, migrating east and north into areas previously covered by Dc and Ec.
- Steppe (BS) and Mediterranean (Cs) climate types are projected to expand significantly in southern and southeastern Europe, with BS area expected to double under SSP2-4.5 and triple under SSP5-8.5.
- The desert (BW) climate type is projected to emerge in a small part of southern Spain (approximately 1% of the studied domain) under the higher-emission scenario.
- Climate type boundaries are projected to shift: the Dc/Eo boundary moves northward, and the Do/Dc boundary shows an eastward shift in the second half of the century under higher-emission scenarios.
- The hybrid-CMIP6 dataset generally projects the most pronounced changes, particularly over northern Europe, and a larger increase in dry climate types, reflecting faster temperature changes.
Contributions
- Provides the first assessment of updated CMIP6-based projections of Köppen-Trewartha climate types over Europe using a hybrid GCM-RCM method, anticipating the availability of new EURO-CORDEX simulations dynamically downscaling CMIP6.
- Introduces an innovative and computationally efficient hybrid method that integrates fine-scale RCM information with the climate change signal from the entire GCM ensemble, addressing uncertainties related to the limited number of driving GCMs in RCM ensembles.
- Offers new insights into projected regional changes of KTC climate types, emphasizing uncertainties related to the choice of underlying simulated data (CMIP5 vs. CMIP6, hybrid vs. raw RCMs).
- Generates results directly applicable as a basis for adaptation strategies and planning, and for identifying regions expected to undergo the most dramatic climate changes with implications for vegetation.
Funding
- Johannes Amos Comenius Programme (OP JAC) project No. CZ.02.01.01/00/22_008/0004605, Natural and anthropogenic georisk.
Citation
@article{Holtanová2025Scenarios,
author = {Holtanová, Eva and Belda, Michal and Randriatsara, Herijaona Hani‐Roge Hundilida and Szabó, Amanda Imola and Halenka, Tomáš},
title = {Scenarios of Köppen-Trewartha climate types in Europe based on GCM-RCM combined projections},
journal = {Theoretical and Applied Climatology},
year = {2025},
doi = {10.1007/s00704-025-05806-3},
url = {https://doi.org/10.1007/s00704-025-05806-3}
}
Original Source: https://doi.org/10.1007/s00704-025-05806-3