globalchange  > 气候变化事实与影响
DOI: 10.5194/hess-23-1833-2019
WOS记录号: WOS:000463350100002
论文题名:
Future evolution and uncertainty of river flow regime change in a deglaciating river basin
作者: Mackay, Jonathan D.1,2; Barrand, Nicholas E.1; Hannah, David M.1; Krause, Stefan1; Jackson, Christopher R.2; Everest, Jez3; Adalgeirsdottir, Gudfinna4; Black, Andrew R.5
通讯作者: Mackay, Jonathan D.
刊名: HYDROLOGY AND EARTH SYSTEM SCIENCES
ISSN: 1027-5606
EISSN: 1607-7938
出版年: 2019
卷: 23, 期:4, 页码:1833-1865
语种: 英语
WOS关键词: CLIMATE-CHANGE IMPACTS ; HAUT-GLACIER-DAROLLA ; MASS-BALANCE ; ACCEPTABILITY FRAMEWORK ; HYDROLOGICAL BEHAVIOR ; MODEL CALIBRATION ; 20-1ST CENTURY ; RUNOFF ; STREAMFLOW ; TEMPERATURE
WOS学科分类: Geosciences, Multidisciplinary ; Water Resources
WOS研究方向: Geology ; Water Resources
英文摘要:

The flow regimes of glacier-fed rivers are sensitive to climate change due to strong climate-cryosphere- hydrosphere interactions. Previous modelling studies have projected changes in annual and seasonal flow magnitude but neglect other changes in river flow regime that also have socio-economic and environmental impacts. This study employs a signature-based analysis of climate change impacts on the river flow regime for the deglaciating Virkisa river basin in southern Iceland. Twenty-five metrics (signatures) are derived from 21st century projections of river flow time series to evaluate changes in different characteristics (magnitude, timing and variability) of river flow regime over sub-daily to decadal timescales. The projections are produced by a model chain that links numerical models of climate and glacio-hydrology. Five components of the model chain are perturbed to represent their uncertainty including the emission scenario, numerical climate model, downscaling procedure, snow/ice melt model and runoff-routing model. The results show that the magnitude, timing and variability of glacier-fed river flows over a range of timescales will change in response to climate change. For most signatures there is high confidence in the direction of change, but the magnitude is uncertain. A decomposition of the projection uncertainties using analysis of variance (ANOVA) shows that all five perturbed model chain components contribute to projection uncertainty, but their relative contributions vary across the signatures of river flow. For example, the numerical climate model is the dominant source of uncertainty for projections of high-magnitude, quick-release flows, while the runoff-routing model is most important for signatures related to low-magnitude, slow-release flows. The emission scenario dominates mean monthly flow projection uncertainty, but during the transition from the cold to melt season (April and May) the snow/ice melt model contributes up to 23 % of projection uncertainty. Signature-based decompositions of projection uncertainty can be used to better design impact studies to provide more robust projections.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/134090
Appears in Collections:气候变化事实与影响

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作者单位: 1.Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England
2.British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England
3.British Geol Survey, Lyell Ctr, Res Ave South, Edinburgh EH14 4AS, Midlothian, Scotland
4.Univ Iceland, Inst Earth Sci, IS-101 Reykjavik, Iceland
5.Univ Dundee, Geog & Environm Sci, Dundee DD1 4HN, Scotland

Recommended Citation:
Mackay, Jonathan D.,Barrand, Nicholas E.,Hannah, David M.,et al. Future evolution and uncertainty of river flow regime change in a deglaciating river basin[J]. HYDROLOGY AND EARTH SYSTEM SCIENCES,2019-01-01,23(4):1833-1865
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