The cumulative effects of forest disturbance and climate variability on streamflow components in a large forest-dominated watershed

被引:53
作者
Li, Qiang [1 ]
Wei, Xiaohua [1 ]
Zhang, Mingfang [2 ]
Liu, Wenfei [3 ]
Giles-Hansen, Krysta [1 ]
Wang, Yi [1 ]
机构
[1] Univ British Columbia Okanagan, Dept Earth Environm & Geog Sci, 1177 Res Rd, Kelowna, BC V1V 1V7, Canada
[2] Univ Elect Sci & Technol China, Sch Resources & Environm, 2006 Xiyuan Ave, Chengdu 611731, Sichuan, Peoples R China
[3] Nanchang Inst Technol, Inst Ecol & Environm Sci, Nanchang, Jiangxi, Peoples R China
基金
加拿大自然科学与工程研究理事会;
关键词
Forest disturbance; Climate variability; Baseflow separation; Relative contributions; Streamflow components; Cumulative effects; CONDUCTIVITY MASS-BALANCE; LAND-USE CHANGE; HYDROLOGICAL RESPONSES; GROUNDWATER RECHARGE; HYDROGRAPH SEPARATION; BASEFLOW SEPARATION; NEW-BRUNSWICK; RIVER; CATCHMENT; YIELD;
D O I
10.1016/j.jhydrol.2017.12.056
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Assessing how forest disturbance and climate variability affect streamflow components is critical for watershed management, ecosystem protection, and engineering design. Previous studies have mainly evaluated the effects of forest disturbance on total streamflow, rarely with attention given to its components (e.g., base flow and surface runoff), particularly in large watersheds (>1000 km(2)). In this study, the Upper Similkameen River watershed (1810 km(2)), an international watershed situated between Canada and the USA, was selected to examine how forest disturbance and climate variability interactively affect total streamflow, baseflow, and surface runoff. Baseflow was separated using a combination of the recursive digital filter method and conductivity mass balance method. Time series analysis and modified double mass curves were then employed to quantitatively separate the relative contributions of forest disturbance and climate variability to each streamflow component. Our results showed that average annual baseflow and baseflow index (baseflow/streamflow) were 113.3 +/- 35.6 mm year(-1) and 0.27 for 1954-2013, respectively. Forest disturbance increased annual streamflow, baseflow, and surface runoff of 27.7 +/- 13.7 mm, 7.4 +/- 3.6 mm, and 18.4 +/- 12.9 mm, respectively, with its relative contributions to the changes in respective streamflow components being 27.0 +/- 23.0%, 29.2 +/- 23.1%, and 25.7 +/- 23.4%, respectively. In contrast, climate variability decreased them by 74.9 +/- 13.7 mm, 17.9 +/- 3.6 mm, and 53.3 +/- 12.9 mm, respectively, with its relative contributions to the changes in respective streamflow components being 73.0 +/- 23.0%, 70.8 +/- 23.1% and 73.1 +/- 23.4%, respectively. Despite working in opposite ways, the impacts of climate variability on annual streamflow, baseflow, and surface runoff were of a much greater magnitude than forest disturbance impacts. This study has important implications for the protection of aquatic habitat, engineering design, and watershed planning in the context of future forest disturbance and climate change. (C) 2017 Elsevier B.V. All rights reserved.
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页码:448 / 459
页数:12
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