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Exploring the role of hydrological pathways in modulating multi-annual climate teleconnection periodicities from UK rainfall to streamflow

机译:探讨水文途径在调制英国降雨中调制多年度气候拨电话周期的作用

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An understanding of multi-annual behaviour in streamflow allows for better estimation of the risks associated with hydrological extremes. This can enable improved preparedness for streamflow-dependant services, such as freshwater ecology, drinking water supply and agriculture. Recently, efforts have focused on detecting relationships between long-term hydrological behaviour and oscillatory climate systems (such as the North Atlantic Oscillation – NAO). For instance, the approximate 7?year periodicity of the NAO has been detected in groundwater-level records in the North Atlantic region, providing potential improvements to the preparedness for future water resource extremes due to their repetitive, periodic nature. However, the extent to which these 7-year, NAO-like signals are propagated to streamflow, and the catchment processes that modulate this propagation, are currently unknown. Here, we show statistically significant evidence that these 7-year periodicities are present in streamflow (and associated catchment rainfall), by applying multi-resolution analysis to a large data set of streamflow and associated catchment rainfall across the UK. Our results provide new evidence for spatial patterns of NAO periodicities in UK rainfall, with areas of greatest NAO signal found in southwest England, south Wales, Northern Ireland and central Scotland, and show that NAO-like periodicities account for a greater proportion of streamflow variability in these areas. Furthermore, we find that catchments with greater subsurface pathway contribution, as characterised by the baseflow index (BFI), generally show increased NAO-like signal strength and that subsurface response times (as characterised by groundwater response time – GRT), of between 4 and 8 years, show a greater signal presence. Our results provide a foundation of understanding for the screening and use of streamflow teleconnections for improving the practice and policy of long-term streamflow resource management.
机译:对流流中的多年度行为的理解允许更好地估计与水文极端相关的风险。这可以改进的流出依赖性服务的准备,例如淡水生态,饮用水和农业。最近,努力专注于检测长期水文行为和振荡气候系统(如北大西洋振荡 - Nao)之间的关系。例如,在北大西洋地区的地下水位记录中检测到NAO的近似值,由于它们的重复,周期性,因此对未来水资源极端的准备进行了潜在的改进。然而,这7年,Nao样信号传播到流流的程度,以及调制该传播的集水过程目前未知。在这里,我们展示了统计上的重要证据,即通过将多分辨率分析应用于英国的大型数据集和相关的集水区降雨,这些7年期限性存在于流流(和相关的集水区降雨)中。我们的结果为英国南威尔士州西南部,南威尔士州,北爱尔兰和中央苏格兰中发现的Nao周期性的空间模式提供了新的证据。在这些领域。此外,我们发现具有更高的地下途径贡献的集水区,如基流指数(BFI)所表征,通常显示出增加的Nao样信号强度,并且该地下响应时间(如地下水响应时间 - GRT的特征在一起)之间的4个和8年,显示出更大的信号存在。我们的结果为筛查和使用流式电信连接提供了了解,为改善长期流流程资源管理的实践和政策提供了理解。

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