EGU26-6552, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-6552
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 14:18–14:21 (CEST)
 
vPoster spot 4
Poster | Tuesday, 05 May, 16:15–18:00 (CEST), Display time Tuesday, 05 May, 14:00–18:00
 
vPoster Discussion, vP.84
Assessing future wind energy resources in the Iberian Peninsula under climate change scenarios
Alonso García-Miguel1, Carlos Calvo Sancho2,3, Javier Díaz Fernández2,4, Juan Jesús González Alemán4, Mauricio López Reyes5,6, Pedro Bolgiani5, María Luisa Martín Pérez2,7, and María Yolanda Luna4
Alonso García-Miguel et al.
  • 1Department of Automation, Electrical and Electronic Engineering and Industrial Computing, Universidad Politécnica de Madrid, Spain (alogarmi01@gmail.com)
  • 2Department of Applied Mathematics, Faculty of Computer Engineering, Universidad de Valladolid, Spain
  • 3Centro de Investigaciones sobre Desertificación, Consejo Superior de Investigaciones Científicas (CIDE, CSIC-UV-GVA), Climate, Atmosphere and Ocean Laboratory (Climatoc-Lab), Moncada, Valencia, Spain
  • 4Agencia Estatal de Meteorología (AEMET), Spain
  • 5Department of Earth Physics and Astrophysics, Faculty of Physics, Complutense University of Madrid, Madrid, Spain
  • 6Instituto de Astronomía y Meteorología (IAM), Departamento de Física, Centro Universitario de Ciencias Exactas e Ingenierías, Universidad de Guadalajara, Guadalajara, México
  • 7Interdisciplinary Mathematics Institute, Universidad Complutense de Madrid, Spain

This study evaluates annual changes in wind power density (WPD) in a domain covering the Iberian Peninsula and adjacent areas using several CMIP6 global climate models and the ensemble mean under historical (1961-1990) and SSP5-8.5 scenarios for two-time horizons—near future (2041–2070) and far future (2071–2100).

Results from the ensemble indicate a robust and generalized decrease in WPD throughout the 21st century. The most pronounced declines occur in windows starting mid-century (2050–2055), with reductions of about -90 W m-2 century-1 persisting for up to 40-year periods. Short-lived positive trends (≈ 50 W m-2 century-1) appear around 2030 and 2045, suggesting temporary peaks before a marked decline (≈ -100 W m-2 century-1) in later decades. Comparisons between future and historical periods reveal strong WPD decreases (-70 W m-2), mainly offshore, particularly in far-future scenarios.

Inland areas may experience annual mean WPD values falling below the cut-in threshold (3 m/s, ≈ 15.5 W m-2), rendering some older wind farms economically and technically unviable. Offshore regions, despite current technological priorities, face substantial WPD reductions (up to -60 W m-2), while inland declines are significant in northeastern Spain, where major wind farms are located. These projected reductions—especially offshore (10–20%)—could challenge the financial viability of future wind energy projects.

How to cite: García-Miguel, A., Calvo Sancho, C., Díaz Fernández, J., González Alemán, J. J., López Reyes, M., Bolgiani, P., Martín Pérez, M. L., and Luna, M. Y.: Assessing future wind energy resources in the Iberian Peninsula under climate change scenarios, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-6552, https://doi.org/10.5194/egusphere-egu26-6552, 2026.