Natural flood management, lag time and catchment scale: Results from an empirical nested catchment study

被引:41
作者
Black, Andrew [1 ]
Peskett, Leo [2 ]
MacDonald, Alan [1 ,3 ]
Young, Andy [1 ,4 ]
Spray, Chris [1 ]
Ball, Tom [5 ]
Thomas, Huw [6 ]
Werritty, Alan [1 ]
机构
[1] Univ Dundee, Geog & Environm Sci, Dundee DD1 4HN, Scotland
[2] Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland
[3] British Geol Survey, Lyell Ctr, Edinburgh, Midlothian, Scotland
[4] Wallingford HydroSolut, Wallingford, Oxon, England
[5] Univ Winchester, Dept Archaeol Anthropol & Geog, Winchester, Hants, England
[6] Talybont Res Off, Ctr Ecosyst Soc & Biosecur, Forest Res, Talybont On Usk, Wales
关键词
catchment scale; Eddleston; empirical analysis; lag; natural flood management; BELFORD CATCHMENT; RISK-MANAGEMENT;
D O I
10.1111/jfr3.12717
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Natural flood management (NFM) techniques attract much interest in flood risk management science, not least because their effectiveness remains subject to considerable uncertainty, particularly at larger catchment and event scales. This derives from a paucity of empirical studies which can offer either longitudinal or comparison data sets in which changes can be observed. The Eddleston catchment study, with 13 stream gauges operated continuously over 9 years, is based on both longitudinal and comparison data sets. Two years of baseline monitoring have been followed by 7 years of further monitoring after a range of NFM interventions across the 69 km(2) catchment. This study has examined changes in lag as an index of hydrological response which avoids dependence on potentially significant uncertainties in flow data. Headwater catchments up to 26 km(2) showed significant delays in lag of 2.6-7.3 hr in catchments provided with leaky wood structures, on-line ponds and riparian planting, while larger catchments downstream and those treated with riparian planting alone did not. Two control catchments failed to show any such changes. The findings provide important evidence of the catchment scale at which NFM can be effective and suggest that effects may increase with event magnitude.
引用
收藏
页数:16
相关论文
共 70 条
[31]   Natural flood management [J].
Lane, Stuart N. .
WILEY INTERDISCIPLINARY REVIEWS-WATER, 2017, 4 (03)
[32]   Velocity and flow resistance in step-pool streams [J].
Lee, AJ ;
Ferguson, RI .
GEOMORPHOLOGY, 2002, 46 (1-2) :59-71
[33]  
Lewis G.L., 2002, INTRO HYDROLOGY, P624
[34]   Physically-based estimation of lag time for forested mountainous watersheds [J].
Loukas, A ;
Quick, MC .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 1996, 41 (01) :1-19
[35]   Uncertainty Analyses of Watershed Time Parameters [J].
McCuen, Richard H. .
JOURNAL OF HYDROLOGIC ENGINEERING, 2009, 14 (05) :490-498
[36]  
McCuen Richard H., 2005, Hydrologic analysis and design, V3
[37]  
Metcalfe P., 2017, SIMPLIFIED REPRESENT
[38]   A modelling framework for evaluation of the hydrological impacts of nature-based approaches to flood risk management, with application to in-channel interventions across a 29-km2 scale catchment in the United Kingdom [J].
Metcalfe, Peter ;
Beven, Keith ;
Hankin, Barry ;
Lamb, Rob .
HYDROLOGICAL PROCESSES, 2017, 31 (09) :1734-1748
[39]  
Ncube Sikhululekile, 2018, International Journal of Biodiversity Science Ecosystem Services & Management, V14, P145, DOI 10.1080/21513732.2018.1489306
[40]   Runoff attenuation features: a sustainable flood mitigation strategy in the Belford catchment, UK [J].
Nicholson, A. R. ;
Wilkinson, M. E. ;
O'Donnell, G. M. ;
Quinn, P. F. .
AREA, 2012, 44 (04) :463-469