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首页> 外文期刊>Journal of Hydrology >The impact of droughts and water management on various hydrological systems in the headwaters of the Tagus River (central Spain)
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The impact of droughts and water management on various hydrological systems in the headwaters of the Tagus River (central Spain)

机译:干旱和水资源管理对塔霍河上游水域各种水文系统的影响(西班牙中部)

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The influence of climate variation on the availability of water resources was analyzed in the headwaters of the Tagus River basin using two drought indices, the standardized precipitation index (SPI) and the standardized precipitation evapotranspiration index (SPEI). This basin is highly regulated and strategic, and contains two hyperannual reservoirs that are the origin of the water supply system for Mediterranean areas of southeast Spain. The indices confirmed that drought conditions have prevailed in the headwaters of the Tagus River since the 1970s. The responses in river discharge and reservoir storage were slightly higher when based on the SPEI rather than the SPI, which indicates that although precipitation had a major role in explaining temporal variability in the analyzed parameters, the influence of temperature was not negligible. Moreover, the greatest response in hydrological variables was evident over longer timescales of the climatic drought indices. Although the effect of climate variability on water resources was substantial during the analyzed period, we also showed a major change in hydrological-climatic relationships in regulated systems including reservoir storage and outflow. These were closely related to changes in external demand following commencement of the water transfer system to the Júcar and Segura basins after the 1980s. The marked reduction in water availability in the basin, which is related to more frequent droughts, contrasts with the amount of water transferred, which shows a clear upward trend associated with increasing water demand in the Mediterranean basin.
机译:利用两个干旱指数,即标准降水指数(SPI)和标准降水蒸散指数(SPEI),分析了塔霍河流域源头气候变化对水资源可用性的影响。该流域受到高度管制和战略控制,并包含两个多年生水库,它们是西班牙东南部地中海地区供水系统的起源。这些指数证实,自1970年代以来塔霍河的源头一直存在干旱条件。当基于SPEI而不是SPI时,河流流量和水库存储的响应略高,这表明尽管降水在解释所分析参数的时间变化方面起主要作用,但温度的影响不可忽略。此外,在更长的气候干旱指数范围内,水文变量的最大响应是显而易见的。尽管在分析期间气候变异性对水资源的影响很大,但我们还显示了包括储水库和出库在内的调节系统中水文-气候关系的重大变化。这些与1980年代后开始向尤卡尔和塞古拉盆地的输水系统启动后外部需求的变化密切相关。流域的可用水量明显减少,这与干旱的频繁发生有关,这与转移的水量形成了鲜明的对比,后者表明与地中海流域的需水量增加明显相关的上升趋势。

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