Department of Applied Physics, University of Granada, Campus Fuente Nueva S/N, ES18071 Granada, Spain.
Department of Applied Physics, University of Granada, Campus Fuente Nueva S/N, ES18071 Granada, Spain.
Sci Total Environ. 2020 Jun 20;722:137902. doi: 10.1016/j.scitotenv.2020.137902. Epub 2020 Mar 12.
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 high-resolution 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 21 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 during winter, 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 on water 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.
这项工作研究了干湿气候过渡地区,即伊比利亚半岛(IP)的气候变化预测。为此,使用了经过先前偏差校正的两个全球气候模型(CCSM4 和 MPI-ESM-LR)驱动的天气研究和预报(WRF)模型,以生成高分辨率的气候信息。模拟分为两个时期进行,分别为 1980-2014 年和 2071-2100 年,以及两种代表性浓度途径(RCP4.5 和 RCP8.5)。分析重点是陆面过程的变化、其原因以及对气候系统的潜在影响。为了实现这一目标,研究了与水文(即降水和径流量)和能量平衡(即温度和太阳入射辐射)相关的陆面(土壤湿度和地表蒸散)和大气变量的季节性预测变化。结果表明,到 21 世纪末,IP 可能会经历土壤干燥,特别是在夏季和秋季,在 IP 南部更为明显,在 RCP8.5 下更为强烈。然而,这些趋势在全年会有不同的影响,并直接影响地表蒸散。此外,土壤干燥趋势主要与春季、夏季和秋季大规模降水减少以及西北 IP 地区春季蒸散增强有关。此外,结果显示高海拔地区土壤条件发生显著变化,特别是在冬季,这可能会改变目前在这些地区发生的陆气过程。在这种情况下,预计气候系统会发生显著变化,从而对水资源和温度产生不利影响。研究结果突出了像 IP 这样的地区陆气相互作用的复杂和非线性性质,这对充分制定缓解和适应人为气候变化的策略构成了巨大挑战。