Storylines of projected summer warming in Iberia using atmospheric circulation, soil moisture and sea surface temperature as drivers of uncertainty

• Published in: Atmospheric research Vol. 311; p. 107677
• Main Authors: Garrido-Perez, Jose M., Barriopedro, David, Trigo, Ricardo M., Soares, Pedro M.M., Zappa, Giuseppe, Álvarez-Castro, M. Carmen, García-Herrera, Ricardo
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.12.2024
• Subjects: Climate change; CMIP6; Europe; Heatwave; Land-atmosphere; Regional; Land-atmosphere; Climate change; CMIP6; Heatwave; Regional; Europe
• ISSN: 0169-8095
• DOI: 10.1016/j.atmosres.2024.107677

This study explores the uncertainty of future summer warming over Iberia using storylines constructed from climate model simulations of the Climate Model Intercomparison Project Phase 6. Unlike prior storyline approaches focusing on remote drivers and global teleconnections of atmospheric circulation, we use regional factors that directly influence summer temperatures: ridging activity, soil moisture and Mediterranean sea surface temperature. These drivers explain a substantial portion of the observed variability across climate models, with ridging activity and soil moisture showing the strongest influence on Iberian warming. Under a high radiative forcing scenario (SSP5–8.5), the storylines of Iberian warming based on these two drivers range between 7 and 9 °C for the end of the 21st century. The storyline leading to the largest warming is characterised by a drying out of the soil conditions and an increase in the anticyclonic activity over Iberia. We find similar conclusions for simple extreme heat indicators, though the approach struggles with more complex heatwave metrics. We also propose a novel modification of the storyline approach to increase the data sample of climate responses by using different time intervals throughout the 21st century. This modification would allow the application of more complex statistical models, the exploration of non-linear relationships and the identification of other drivers shaping the regional climate projections. •Soil moisture & ridging explain most multi-model spread of Iberian warming (IW).•Storylines of IW range between ∼1.6–2.1 °C per degree of global warming.•The influence of Mediterranean sea surface temperatures on IW is of secondary importance.•Similar findings on extreme temperatures, but complex metrics pose challenges.•Novel modification of the storyline approach: extending data via moving windows.