0619487 - ÚVGZ 2026 RIV US eng J - Journal Article
Skalák, Petr - Meitner, Jan - Fischer, Milan - Orság, Matěj - Graf, A. - Hlavsová, Monika - Trnka, Miroslav
The Projected Changes in the Surface Energy Budget of the CMIP5 and EURO-CORDEX Models: Are We Heading toward Wetter Growing Seasons in Central Europe?
Journal of Hydrometeorology. Roč. 26, č. 4 (2025), s. 481-499. ISSN 1525-755X. E-ISSN 1525-7541
R&D Projects: GA MŠMT(CZ) EH22_008/0004635; GA ČR(CZ) GA24-12935S
Institutional support: RVO:86652079
Keywords : climate * trends * Europe * Climate change * Energy budget/balance * Climate models
OECD category: Meteorology and atmospheric sciences
Impact factor: 3.1, year: 2023 ; AIS: 1.218, rok: 2023
Method of publishing: Open access
Result website:
https://journals.ametsoc.org/view/journals/hydr/26/4/JHM-D-24-0017.1.xmlDOI: https://doi.org/10.1175/JHM-D-24-0017.1

We analyze the surface energy budget from four climate model ensembles and its future changes in the twenty-first century under the RCP8.5 or shared socioeconomic pathway (SSP) 5-8.5 scenario. High-resolution European domain of the Coordinated Regional Climate Downscaling Experiment (EURO-CORDEX) regional climate models (RCMs) and their driving CMIP5 global climate models (CMIP5-D) are first tested in central Europe against observational datasets. Evaluation reveals the added value of RCMs in terms of spatial variability and smaller biases. CMIP5-D are affected by the positive bias of global irradiance that propagates into other radiation and heat fluxes. There are strong differences in the projected surface energy budget components between RCMs and CMIP5-D. There is an increase in global irradiance for most of the year in CMIP5-D and other GCM ensembles that is translated into a year-round enhancement of the absorbed solar energy and balanced by higher latent heat flux, except in summer, when the sensible heat flux rises strongly. Together with strong warming and reduced precipitation in summer, this leads to warm, sunny, and dry conditions with reduced evapotranspiration and higher drought stress for vegetation. In the RCMs, the reduction in global irradiance dominates, and it is translated into a round-year reduction in the net balance of longwave radiation and stronger latent heat flux. The first months of the growing season show weaker warming associated with higher evapotranspiration and precipitation. In summer, precipitation drops and global irradiance and warming rise, but they fall behind the changes in the GCMs. Compared to GCMs, there are less visible signs of conditions leading to a reduction in evapotranspiration or a shortage of soil water in the RCMs in summer.
Permanent Link: https://hdl.handle.net/11104/0367807