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首页> 外文期刊>Science of the total environment >Does internal climate variability overwhelm climate change signals in streamflow? The upper Po and Rhone basin case studies
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Does internal climate variability overwhelm climate change signals in streamflow? The upper Po and Rhone basin case studies

机译:内部气候变化是否会淹没河流中的气候变化信号?上波河和罗纳河盆地案例研究

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摘要

Projections of climate change effects in streamflow are increasingly required to plan water management strategies. These projections are however largely uncertain due to the spread among climate model realizations, internal climate variability, and difficulties in transferring climate model results at the spatial and temporal scales required by catchment hydrology. A combination of a stochastic downscaling methodology and distributed hydrological modeling was used in the ACQWA project to provide projections of future streamflow (up to year 2050) for the upper Po and Rhone basins, respectively located in northern Italy and south-western Switzerland. Results suggest that internal (stochastic) climate variability is a fundamental source of uncertainty, typically comparable or larger than the projected climate change signal. Therefore, climate change effects in streamflow mean, frequency, and seasonality can be masked by natural climatic fluctuations in large parts of the analyzed regions. An exception to the overwhelming role of stochastic variability is represented by high elevation catchments fed by glaciers where streamflow is expected to be considerably reduced due to glacier retreat, with consequences appreciable in the main downstream rivers in August and September. Simulations also identify regions (west upper Rhone and Toce, Ticino river basins) where a strong precipitation increase in the February to April period projects streamflow beyond the range of natural climate variability during the melting season. This study emphasizes the importance of including internal climate variability in climate change analyses, especially when compared to the limited uncertainty that would be accounted for by few deterministic projections. The presented results could be useful in guiding more specific impact studies, although design or management decisions should be better based on reliability and vulnerability criteria as suggested by recent literature.
机译:为了规划水管理策略,越来越需要对水流中的气候变化影响进行预测。但是,由于气候模型认识之间的差异,内部气候的可变性以及流域水文学所需的时空尺度上传递气候模型结果的困难,这些预测在很大程度上不确定。 ACQWA项目将随机缩减规模方法和分布式水文模型相结合,为分别位于意大利北部和瑞士西南部的Po盆地和Rhone盆地的未来水流(到2050年)提供了预测。结果表明,内部(随机)气候变化是不确定性的基本来源,通常比预期的气候变化信号可比或更大。因此,被分析区域大部分地区的自然气候波动可以掩盖气候变化对流量平均值,频率和季节性的影响。随机变异性发挥压倒性作用的一个例外是冰川给水造成的高海拔集水区,由于冰川的退缩,预计河流流量将大大减少,其后果在八月和九月的主要下游河流明显。模拟还确定了区域(罗纳河上游和托斯河,提契诺州流域),在二月至四月期间降水增加强烈,导致河流流量超出了融化季节自然气候变化范围。这项研究强调了将内部气候变异性纳入气候变化分析的重要性,特别是与很少的确定性预测所能解释的有限不确定性相比。尽管根据近期文献所建议的可靠性和脆弱性标准,设计或管理决策应该更好,但提出的结果可能有助于指导更具体的影响研究。

著录项

  • 来源
    《Science of the total environment》 |2014年第15期|1171-1182|共12页
  • 作者单位

    Institute of Environmental Engineering, ETH Zuerich, Stefano Franscini-Platz 5, HIL D 23.2,8093 Zuerich, Switzerland;

    Institute of Environmental Engineering, ETH Zuerich, Stefano Franscini-Platz 5, HIL D 23.2,8093 Zuerich, Switzerland;

    Institute of Environmental Engineering, ETH Zuerich, Stefano Franscini-Platz 5, HIL D 23.2,8093 Zuerich, Switzerland;

    Institute of Environmental Engineering, ETH Zuerich, Stefano Franscini-Platz 5, HIL D 23.2,8093 Zuerich, Switzerland;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; Hydrological modeling; Stochastic downscaling; Uncertainty; Water resources; Alps;

    机译:气候变化;水文模拟;随机缩减不确定;水资源;阿尔卑斯山;

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