globalchange  > 气候变化事实与影响
DOI: 10.5194/hess-19-2469-2015
Scopus记录号: 2-s2.0-84930224749
论文题名:
Shallow groundwater thermal sensitivity to climate change and land cover disturbances: Derivation of analytical expressions and implications for stream temperature modeling
作者: Kurylyk B; L; , MacQuarrie K; T; B; , Caissie D; , McKenzie J; M
刊名: Hydrology and Earth System Sciences
ISSN: 10275606
出版年: 2015
卷: 19, 期:5
起始页码: 2469
结束页码: 2489
语种: 英语
Scopus关键词: Advection ; Aquifers ; Atmospheric temperature ; Groundwater ; Groundwater resources ; Heat flux ; Logging (forestry) ; Rivers ; Sensitivity analysis ; Surface measurement ; Surface properties ; Advection-diffusion equation ; Air temperature variations ; Analytical expressions ; Groundwater temperatures ; Land surface temperature ; Long-term variability ; Stream temperature models ; Surface perturbations ; Climate change ; advection-diffusion equation ; air temperature ; aquatic community ; aquatic environment ; aquifer ; climate change ; climate modeling ; disturbance ; fish ; global warming ; groundwater ; heat flux ; hydrological modeling ; land cover ; sensitivity analysis ; temperature effect ; timber harvesting ; water temperature
英文摘要: Climate change is expected to increase stream temperatures and the projected warming may alter the spatial extent of habitat for cold-water fish and other aquatic taxa. Recent studies have proposed that stream thermal sensitivities, derived from short-term air temperature variations, can be employed to infer future stream warming due to long-term climate change. However, this approach does not consider the potential for streambed heat fluxes to increase due to gradual warming of the shallow subsurface. The temperature of shallow groundwater is particularly important for the thermal regimes of groundwater-dominated streams and rivers. Also, recent studies have investigated how land surface perturbations, such as wildfires or timber harvesting, can influence stream temperatures by changing stream surface heat fluxes, but these studies have typically not considered how these surface disturbances can also alter shallow groundwater temperatures and streambed heat fluxes.

In this study, several analytical solutions to the one-dimensional unsteady advection-diffusion equation for subsurface heat transport are employed to estimate the timing and magnitude of groundwater temperature changes due to seasonal and long-term variability in land surface temperatures. Groundwater thermal sensitivity formulae are proposed that accommodate different surface warming scenarios. The thermal sensitivity formulae suggest that shallow groundwater will warm in response to climate change and other surface perturbations, but the timing and magnitude of the subsurface warming depends on the rate of surface warming, subsurface thermal properties, bulk aquifer depth, and groundwater velocity. The results also emphasize the difference between the thermal sensitivity of shallow groundwater to short-term (e.g., seasonal) and long-term (e.g., multi-decadal) land surface-temperature variability, and thus demonstrate the limitations of using short-term air and water temperature records to project future stream warming. Suggestions are provided for implementing these formulae in stream temperature models to accommodate groundwater warming. © 2015 Author(s).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/78513
Appears in Collections:气候变化事实与影响

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作者单位: University of New Brunswick, Department of Civil Engineering, Canadian Rivers Institute, Fredericton, NB, Canada; Fisheries and Oceans Canada, Gulf Fisheries Centre, Moncton, NB, Canada; McGill University, Department of Earth and Planetary Sciences, McGill University, Montreal, QC, Canada; University of Calgary, Department of Geoscience, Calgary, AB, Canada

Recommended Citation:
Kurylyk B,L,, MacQuarrie K,et al. Shallow groundwater thermal sensitivity to climate change and land cover disturbances: Derivation of analytical expressions and implications for stream temperature modeling[J]. Hydrology and Earth System Sciences,2015-01-01,19(5)
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