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Published on: January 7, 2019
Projected changes in the Iberian Peninsula drought characteristics
Matilde García-Valdecasas Ojeda1, Sonia Raquel Gámiz-Fortis2, Emilio Romero-Jiménez2
1Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain; Istituto Nazionale di Oceanografia e di Geosica Sperimentale (OGS), Borgo Grotta Gigante, 42/c, TS34010 Sgonico, Italy; Earth System Physics Section, International Centre for Theoretical Physics (ICTP), Strada Costiera, 11, TS34151 Trieste, Italy.
The Iberian Peninsula faces increasingly severe and prolonged droughts, with a significant risk of megadroughts by 2100 under high-emission scenarios. Projections show intensified drought conditions, especially when using the Standardized Precipitation Evapotranspiration Index (SPEI).
Area of Science:
- Climate Science
- Environmental Science
- Hydrology
Background:
- Droughts pose a significant threat to the Iberian Peninsula (IP).
- Understanding future drought characteristics is crucial for adaptation strategies.
- Previous projections often lack high spatial resolution.
Purpose of the Study:
- To project high spatial resolution drought characteristics for the Iberian Peninsula.
- To analyze changes in drought duration, frequency, and severity under different climate scenarios.
- To compare the performance of two drought indices in capturing these changes.
Main Methods:
- Utilized the Weather Research and Forecasting (WRF) model for regional climate simulations.
- Drove WRF with two Global Climate Models (CCSM4 and MPI-ESM-LR).
- Analyzed drought using Standardized Precipitation Evapotranspiration Index (SPEI) and Standardized Precipitation Index (SPI) at 3- and 12-month time scales under RCP4.5 and RCP8.5 scenarios for near (2021-2050) and far (2071-2100) futures.
Main Results:
- The Iberian Peninsula is projected to experience significantly longer and more severe droughts.
- Substantial changes in drought frequency, duration, and severity are expected across most of the IP by the end of the century, particularly under RCP8.5.
- The SPEI indicated more severe drought increases than the SPI, especially under high-emission scenarios, with a notable risk of megadroughts ( >15 years) by 2100.
Conclusions:
- Climate change will likely intensify drought conditions in the Iberian Peninsula.
- The choice of drought index (SPEI vs. SPI) influences the projected severity and risk, with SPEI showing more extreme outcomes.
- Urgent mitigation and adaptation measures are needed to address the escalating risk of severe and prolonged droughts, including potential megadroughts.
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