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Likely effects of climate change on groundwater availability in a Mediterranean region of Southeastern Spain

机译:气候变化可能对西班牙东南部地中海地区的地下水供应产生影响

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摘要

Groundwater resources are typically the main fresh water source in arid and semi-arid regions. Natural recharge of aquifers is mainly based on precipitation; however, only heavy precipitation events (HPEs) are expected to produce appreciable aquifer recharge in these environments. In this work, we used daily precipitation and monthly water level time series from different locations over a Mediterranean region of Southeastern Spain to identify the critical threshold value to define HPEs that lead to appreciable aquifer recharge in this region. Wavelet and trend analyses were used to study the changes in the temporal distribution of the chosen HPEs (=20¿mm¿day-1) over the observed period 1953–2012 and its projected evolution by using 18 downscaled climate projections over the projected period 2040–2099. The used precipitation time series were grouped in 10 clusters according to similarities between them assessed by using Pearson correlations. Results showed that the critical HPE threshold for the study area is 20¿mm¿day-1. Wavelet analysis showed that observed significant seasonal and annual peaks in global wavelet spectrum in the first sub-period (1953–1982) are no longer significant in the second sub-period (1983–2012) in the major part of the ten clusters. This change is because of the reduction of the mean HPEs number, which showed a negative trend over the observed period in nine clusters and was significant in five of them. However, the mean size of HPEs showed a positive trend in six clusters. A similar tendency of change is expected over the projected period. The expected reduction of the mean HPEs number is two times higher under the high climate scenario (RCP8.5) than under the moderate scenario (RCP4.5). The mean size of these events is expected to increase under the two scenarios. The groundwater availability will be affected by the reduction of HPE number which will increase the length of no aquifer recharge periods (NARP) accentuating the groundwater drought in the region. Copyright © 2016 John Wiley & Sons, Ltd.
机译:地下水资源通常是干旱和半干旱地区的主要淡水来源。含水层的自然补给主要是基于降水。但是,在这些环境中,只有强降水事件(HPE)才能产生可​​观的含水层补给。在这项工作中,我们使用了西班牙东南部地中海地区不同位置的每日降水量和每月水位时间序列来确定临界阈值,以定义可导致该地区明显含水层补给的HPE。通过使用小波和趋势分析来研究选定的HPE的时间分布(= 20?mm?day-1)在1953-2012年观测期间的变化及其预测演变,方法是使用2040年预测期间的18个按比例缩小的气候预测–2099。根据使用Pearson相关性评估的相似度,将使用的降水时间序列分为10个类。结果表明,该研究区域的关键HPE阈值为20?mm?day-1。小波分析表明,在十个聚类的大部分中,在第一子时段(1953-1982年)观测到的全球小波谱的明显季节性和年度峰值在第二子时段(1983-2012年)不再显着。这种变化是由于平均HPE数量的减少所致,该数量在观察到的时期内呈消极趋势,出现在九个集群中,其中五个集群表现显着。但是,HPE的平均规模在六个集群中呈正趋势。在预计的时期内,预计会有类似的变化趋势。在高气候情景(RCP8.5)下,预期的平均HPE数量减少是在中等气候情景(RCP4.5)下的两倍。在两种情况下,这些事件的平均大小预计会增加。 HPE数量的减少将影响地下水的可利用性,这将增加无水层补给期(NARP)的持续时间,加剧该地区的地下水干旱。版权所有©2016 John Wiley&Sons,Ltd.

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