A preliminary assessment of water partitioning and ecohydrological coupling in northern headwaters using stable isotopes and conceptual runoff models

被引:59
作者
Tetzlaff, Doerthe [1 ]
Buttle, James [2 ]
Carey, Sean K. [3 ]
van Huijgevoort, Marjolein H. J. [1 ]
Laudon, Hjalmar [4 ]
McNamara, James P. [5 ]
Mitchell, Carl P. J. [6 ]
Spence, Chris [7 ]
Gabor, Rachel S. [1 ]
Soulsby, Chris [1 ]
机构
[1] Univ Aberdeen, Sch Geosci, Northern Rivers Inst, Aberdeen AB24 3UF, Scotland
[2] Trent Univ, Dept Geog, Peterborough, ON K9J 7B8, Canada
[3] McMaster Univ, Sch Geog & Earth Sci, Hamilton, ON L8S 4K1, Canada
[4] Swedish Univ Agr Sci, Dept Forest Ecol & Management, SE-90183 Umea, Sweden
[5] Boise State Univ, Dept Geosci, Boise, ID 83725 USA
[6] Univ Toronto Scarborough, Dept Phys & Environm Sci, Toronto, ON M1C 1A4, Canada
[7] Environm Canada, Natl Hydrol Res Ctr, Saskatoon, SK S7N 3H5, Canada
基金
欧洲研究理事会; 美国国家科学基金会; 加拿大自然科学与工程研究理事会;
关键词
stable isotopes; water partitioning; cold regions; ecohydrology; CATCHMENT TRANSIT-TIME; SOIL-WATER; LANDSCAPE CHARACTERISTICS; GROUNDWATER CONTRIBUTIONS; SPATIAL VARIABILITY; SNOW DISTRIBUTION; CANADIAN SHIELD; GENERATION; DYNAMICS; STORAGE;
D O I
10.1002/hyp.10515
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We combined a conceptual rainfall-runoff model and input-output relationships of stable isotopes to understand ecohydrological influences on hydrological partitioning in snow-influenced northern catchments. Six sites in Sweden (Krycklan), Canada (Wolf Creek; Baker Creek; Dorset), Scotland (Girnock) and theUSA (Dry Creek) span moisture and energy gradients found at high latitudes. A meta-analysis was carried out using the Hydrologiska Byrans Vattenbalansavdelning (HBV) model to estimate the main storage changes characterizing annual water balances. Annual snowpack storage importance was ranked as Wolf Creek > Krycklan > Dorset > Baker Creek > Dry Creek > Girnock. The subsequent rate and longevity of melt were reflected in calibrated parameters that determine partitioning of waters between more rapid and slower flowpaths and associated variations in soil and groundwater storage. Variability of stream water isotopic composition depends on the following: (i) rate and duration of spring snowmelt; (ii) significance of summer/autumn rainfall; and (iii) relative importance of near-surface and deeper flowpaths in routing water to the stream. Flowpath partitioning also regulates influences of summer evaporation on drainage waters. Deviations of isotope data from the Global Meteoric Water Line showed subtle effects of internal catchment processes on isotopic fractionation most likely through evaporation. Such effects are highly variable among sites and with seasonal differences at some sites. After accounting for climate, evaporative fractionation is strongest at sites where lakes and near-surface runoff processes in wet riparian soils can mobilize isotopically enriched water during summer and autumn. Given close soil-vegetation coupling, this may result in spatial variability in soil water isotope pools available for plant uptake. We argue that stable isotope studies are crucial in addressing the many open questions on hydrological functioning of northern environments. (C) 2015 The Authors. Hydrological Processes published by John Wiley & Sons Ltd.
引用
收藏
页码:5153 / 5173
页数:21
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