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

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dc.contributor.author Rust, William
dc.contributor.author Cuthbert, Mark
dc.contributor.author Bloomfield, John
dc.contributor.author Corstanje, Ron
dc.contributor.author Howden, Nicholas
dc.contributor.author Holman, Ian P.
dc.date.accessioned 2021-04-27T15:00:14Z
dc.date.available 2021-04-27T15:00:14Z
dc.date.issued 2021-04-23
dc.identifier.citation Rust W, Cuthbert M, Bloomfield J, et al., (2021) Exploring the role of hydrological pathways in modulating multi-annual climate teleconnection periodicities from UK rainfall to streamflow. Hydrology and Earth System Sciences, Volume 25, Issue 4, April 2021, pp. 2223-2237 en_UK
dc.identifier.issn 1027-5606
dc.identifier.uri https://doi.org/10.5194/hess-25-2223-2021
dc.identifier.uri http://dspace.lib.cranfield.ac.uk/handle/1826/16619
dc.description.abstract 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 en_UK
dc.language.iso en en_UK
dc.publisher European Geosciences Union en_UK
dc.rights Attribution 4.0 International *
dc.rights.uri http://creativecommons.org/licenses/by/4.0/ *
dc.subject North Atlantic Oscillation en_UK
dc.title Exploring the role of hydrological pathways in modulating multi-annual climate teleconnection periodicities from UK rainfall to streamflow en_UK
dc.type Article en_UK


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