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Water availability in a mountainous Andean watershed under CMIP5 climate change scenarios

机译:CMIP5气候变化场景下的山地和海滨流域水资源可用性

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Recent updates to climate change scenarios developed under the Coupled Model Intercomparison Project Phase 5 (CMIP5) are used to compare water resources availability in an Andean mountainous snow-dominated watershed, Maipo en San Alfonso, located in the vicinity of Chile's capital city, Santiago, monthly hydrologic simulations for a base line period and future scenarios are carried out through the software WEAP, considering precipitation and temperature monthly time series predicted for scenarios A2 by GCM MK3.0, as well as for RCPs 2.6 and 8.5 scenarios by GCM MK3.6. Ensembles given by the GCM MK3.6 are used as inputs to the hydrological model to obtain uncertainty of water availability projections. Future hydrological simulations are carried out from years 2011 to 2070. Results show that mean annual flows tend to decrease by 8%, essentially during the snowmelt period for A2 and RCP 8.5 scenarios. Nevertheless for the RCP 2.6 scenario, the tendency to decrease is reversed at the end of the period.
机译:最近在耦合型号互通的项目阶段5(CMIP5)下开发的气候变化方案的更新用于比较Andean Mountain-Snowpinated流域的水资源可用性,位于智利的首都圣地亚哥附近,基本线期和未来情景的每月水文模拟通过软件武器进行,考虑到GCM MK3.0的场景A2预测的降水和温度月度时间序列,以及GCM MK3.6的RCP 2.6和8.5场景。 GCM MK3.6给出的集合用作水文模型的输入,以获得水可用性预测的不确定性。未来的水文模拟从2011年到2070年进行。结果表明,平均年流量往往会在A2和RCP 8.5场景的雪花期间达到8%。然而,对于RCP 2.6场景,减少趋势在该期间结束时逆转。

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