Projected changes in the Iberian Peninsula drought characteristics.

Autor: García-Valdecasas Ojeda M; Department 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. Electronic address: mgvaldecasas@ugr.es., Gámiz-Fortis SR; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: srgamiz@ugr.es., Romero-Jiménez E; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: emiliorj@ugr.es., Rosa-Cánovas JJ; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: jjrc@ugr.es., Yeste P; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: pyeste@ugr.es., Castro-Díez Y; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: ycastro@ugr.es., Esteban-Parra MJ; Department of Applied Physics, University of Granada, Campus Fuentenueva S/N, ES18071 Granada, Spain. Electronic address: esteban@ugr.es.
Jazyk: angličtina
Zdroj: The Science of the total environment [Sci Total Environ] 2021 Feb 25; Vol. 757, pp. 143702. Date of Electronic Publication: 2020 Nov 23.
DOI: 10.1016/j.scitotenv.2020.143702
Abstrakt: High spatial resolution drought projections for the Iberian Peninsula (IP) have been examined in terms of duration, frequency, and severity of drought events. For this end, a set of regional climate simulations was completed using the Weather Research and Forecasting (WRF) model driven by two global climate models (GCMs), the CCSM4 and the MPI-ESM-LR, for a near (2021-2050) and a far (2071-2100) future, and under two representative concentration pathway (RCP) scenarios (RCP4.5 and RCP8.5). Projected changes for these simulations were analyzed using two drought indices, the Standardized Precipitation Evapotranspiration Index (SPEI) and the Standardized Precipitation Index (SPI), considering different time scales (3- and 12-months). The results showed that the IP is very likely to undergo longer and more severe drought events. Substantial changes in drought parameters (i.e., frequency, duration, and severity) were projected by both indices and at both time scales in most of the IP. These changes are particularly strong by the end of the century under RCP8.5. Meanwhile, the intensification of drought conditions is expected to be more moderate for the near future. However, the results also indicated key differences between indices. Projected drought conditions by using the SPEI showed more severe increases in drought events than those from SPI by the end of the century and, especially, for the high-emission scenario. The most extreme conditions were projected in terms of the duration of the events. Specifically, results from the 12-month SPEI analysis suggested a significant risk of megadrought events (drought events longer than 15 years) in many areas of IP by the end of the century under RCP8.5.
Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
(Copyright © 2020 Elsevier B.V. All rights reserved.)
Databáze: MEDLINE