Related Experiment Video
Updated: Nov 26, 2025

Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology
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.
Abstract:
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.
More Related Videos
Related Concept Videos
Responses to Drought and Flooding
Precipitation Processes
Precipitation and Co-precipitation
Adaptations that Reduce Water Loss
Precipitation Gravimetry
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Global Climate Change

