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农业、引水和干旱导致加利利海萎缩。

Agriculture, diversions, and drought shrinking Galilee Sea.

机构信息

Geomorphology and Fluvial Research Group, Ben Gurion University of the Negev, Beer Sheva, Israel.

Israel Oceanographic & Limnological Research, the Kinneret Limnological Laboratory, Migdal 14950, Israel.

出版信息

Sci Total Environ. 2019 Feb 15;651(Pt 1):70-83. doi: 10.1016/j.scitotenv.2018.09.058. Epub 2018 Sep 5.

Abstract

In water-limited regions worldwide, climate change and population growth threaten to desiccate lakes. As these lakes disappear, water managers have often implicated climate change-induced decreases in precipitation and higher temperature-driven evaporative demand-factors out of their control, while simultaneously constructing dams and drilling new wells into aquifers to permit agricultural expansion. One such shrinking lake is the Sea of Galilee (Lake Kinneret), whose decadal mean level has reached a record low, which has sparked heated debate regarding the causes of this shrinkage. However, the relative importance of climatic change, agricultural consumption, and increases in Lebanese water consumption, remain unknown. Here we show that the level of the Sea of Galilee would be stable, even in the face of decreasing precipitation in the Golan Heights. Climatic factors alone are inadequate to explain the record shrinkage of the Sea of Galilee. We found no decreasing trends in inflow from the headwaters of the Upper Jordan River located primarily in Lebanon. Rather, the decrease in discharge of the Upper Jordan River corresponded to a period of expanding irrigated agriculture, doubling of groundwater pumping rates within the basin, and increasing of the area of standing and impounded waters. While rising temperatures in the basin are statistically significant and may increase evapotranspiration, these temperature changes are too small to explain the magnitude of observed streamflow decreases. The results demonstrate that restoring the level of the Sea of Galilee will require reductions in groundwater pumping, surface water diversions, and water consumption by irrigated agriculture.

摘要

在全球水资源短缺的地区,气候变化和人口增长威胁着湖泊的干涸。随着这些湖泊的消失,水资源管理者往往将气候变化导致的降水量减少和更高的温度驱动的蒸发需求归咎于他们无法控制的因素,同时建造水坝并在含水层中钻探新井以允许农业扩张。加利利海(加利利湖)就是这样一个萎缩的湖泊,其十年平均水位已达到历史最低水平,这引发了关于这种收缩原因的激烈争论。然而,气候变化、农业消费以及黎巴嫩用水量增加的相对重要性仍不清楚。在这里,我们表明,即使戈兰高地的降水量减少,加利利海的水位也将保持稳定。仅仅气候因素不足以解释加利利海的创纪录收缩。我们没有发现源自主要位于黎巴嫩的上约旦河源头的入流减少的趋势。相反,上约旦河的流量减少与灌溉农业的扩张时期相对应,流域内地下水抽取率翻了一番,以及静水和蓄水面积的增加。虽然流域内的气温升高具有统计学意义,并且可能增加蒸散量,但这些温度变化太小,无法解释观测到的径流量减少的幅度。研究结果表明,要恢复加利利海的水位,需要减少地下水抽取、地表水引水和灌溉农业的用水量。

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