4.7 Article

Water scarcity down to earth surface in a Mediterranean climate: The extreme future of soil moisture in Portugal

期刊

JOURNAL OF HYDROLOGY
卷 615, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.jhydrol.2022.128731

关键词

Soil moisture; Land water balance; Aridity; Climate change; EURO-CORDEX; Portugal

资金

  1. Pre-defined Project-2 National Roadmap for Adaptation XXI [PDP-2]
  2. Portuguese FCT, I.P./MCTES [UIDB/50019/2020 - IDL]

向作者/读者索取更多资源

Climate change poses a major threat to Mediterranean countries, leading to reduced precipitation, increased temperature, and more frequent extreme events, resulting in water scarcity and various impacts. Portugal, like other Mediterranean countries, already experiences more frequent droughts and soil moisture deficits. Future projections using a multi-model ensemble show a clear reduction in soil moisture throughout the year, due to decreased precipitation and increased evapotranspiration. The study also reveals an increase in soil moisture deficits, especially in the mid-to-end of the century, and a decrease in surface humidity.
Climate change constitutes a major threat for all the Mediterranean countries due to the combination of large precipitation reductions and temperature increases and the higher frequency of climate extremes, especially driving water scarcity and all the derived multi-sectoral impacts. Portugal, as most of the Mediterranean countries, already endures larger frequencies of droughts and deficits in soil moisture and water storage. In the current study, the future projections of soil moisture are examined using a multi-model EURO-CORDEX regional climate ensemble, in agreement with three future emission scenarios (RCP2.6, 4.5 and 8.5). The drivers of future soil moisture dynamics are also analysed and its effect on relative humidity and evaporation rates. As expected, the projections show a clear reduction of soil moisture through the entire annual cycle, in response to the large decrease in precipitation and temperature increase, via a massive growth of potential evapotranspiration. The overall total soil moisture decreases ranges from-5% for the RCP2.6 to-20% (-10%) for the RCP8.5 (RCP4.5), w.r.t. the present climate. In the historical period, soil moisture deficits rarely reach values 3x over the standard deviation, but projections reveal that for the RCP4.5 (RCP8.5) for the mid-century deficits up to 5x (6x) are projected to occur, and for the end-of-century even 7x for the RCP8.5. The annual cycle of soil moisture is in present and future climate determined by precipitation and potential evapotranspiration, and deficit is both enhanced and covers a wider monthly window in the future, especially for the RCP8.5. The surface humidity also decreases importantly, up to-4% and-8% in spring and summer in the end-of-the-century, in agreement with RCP4.5 and RCP8.5, respectively. Resulting from the projected changes in precipitation and potential evapo-transpiration, the typical semi-arid climate, which in present climate is confined to a small south-eastern region of Portugal, is expected to cover almost 2/3 of the mainland in the case of RCP8.5. Finally, this study was developed in the framework of the National Roadmap for Adaptation XXI -Portuguese Territorial Climate Change Vulnerability Assessment for XXI Century (RNA2100) project and aims at delivering a deeper and different featuring of terrestrial water for adaptation purposes in a Mediterranean country.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据