Future changes in land and atmospheric variables: An analysis of their couplings in the Iberian Peninsula

被引:16
|
作者
Garcia-Valdecasas Ojeda, Matilde [1 ]
Yeste, Patricio [1 ]
Raquel Gamiz-Fortis, Sonia [1 ]
Castro-Diez, Yolanda [1 ]
Jesus Esteban-Parra, Maria [1 ]
机构
[1] Univ Granada, Dept Appl Phys, Campus Fuente Nueva S-N, ES-18071 Granada, Spain
关键词
Weather Research and Forecasting; Climate-change projections; Land-surface coupling; Iberian Peninsula; Soil moisture; Surface evapotranspiration; CLIMATE-CHANGE PROJECTIONS; HIGH-RESOLUTION PROJECTIONS; SOIL-MOISTURE; EURO-CORDEX; WATER AVAILABILITY; PART II; PRECIPITATION; MODEL; TEMPERATURE; IMPACT;
D O I
10.1016/j.scitotenv.2020.137902
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This work investigates climate-change projections over a transitional region between dry and wet climates, the Iberian Peninsula (IP). With this purpose, the Weather Research and Forecasting (WRF) model, driven by two global climate models (CCSM4 and MPI-ESM-LR) previously bias-corrected, was used to generate highresolution climate information. Simulations were carried out for two periods, 1980-2014 and 2071-2100, and under two representative concentration pathways (RCP4.5 and RCP8.5). The analysis focused on changes in land-surface processes, their causes, and the potential impact on the climate system. To achieve this, seasonal projected changes of land-surface (soil moisture and surface evapotranspiration) and atmospheric variables involved in the hydrologic (i.e., precipitation and runoff) and energy balance (i.e., temperature and solar incoming radiation) were investigated. The results reveal that the IP is likely to experience a soil dryness by the end of the 21st century, particularly during summer and fall, more apparent in the southern IP, and stronger under the RCP8.5. However, such trends would have different implications throughout the year and directly affect the surface evapotranspiration. Moreover, soil-drying trends are mainly associated with reductions in the large-scale precipitation during spring, summer, and fall and by enhanced evapotranspiration particularly in spring over the northwestern IP. In addition, the results show notably changes in soil conditions at high altitude, particularly duringwinter, which may alter the land-atmosphere processes that currently occur in these regions. In this context, noteworthy changes in the climate system are expected, leading to adverse impacts onwater resources and temperature. The results highlight the complex and nonlinear nature of land-atmosphere interactions in regions such as the IP, which is a tremendous challenge for adequately developing mitigation and adaptation strategies to anthropogenic climate change. (C) 2020 Elsevier B.V. All rights reserved.
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页数:19
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