globalchange  > 气候变化与战略
DOI: 10.5194/hess-22-3421-2018
论文题名:
Hydroclimatic control on suspended sediment dynamics of a regulated Alpine catchment: A conceptual approach
作者: Costa A.; Anghileri D.; Molnar P.
刊名: Hydrology and Earth System Sciences
ISSN: 1027-5606
出版年: 2018
卷: 22, 期:6
起始页码: 3421
结束页码: 3434
语种: 英语
Scopus关键词: Catchments ; Climate change ; Crystallography ; Curve fitting ; Hydroelectric power ; Ice ; Ice control ; Iterative methods ; Nonlinear programming ; Rain ; Reservoirs (water) ; Rhodium compounds ; Runoff ; Sediment transport ; Sedimentation ; Snow ; Snow melting systems ; Fine sediment dynamics ; Hydroclimatic factors ; Hydroclimatic variables ; Hydropower reservoirs ; Nonlinear optimization methods ; Suspended sediment concentrations ; Swiss alpine catchments ; Total suspended sediments ; Suspended sediments ; algorithm ; alpine environment ; catchment ; concentration (composition) ; conceptual framework ; erosion ; hydroelectric power ; hydrometeorology ; optimization ; precipitation (climatology) ; rating curve ; sediment transport ; sediment yield ; snow accumulation ; suspended sediment ; temperature ; Alps ; Rhone Basin ; Switzerland
英文摘要: We analyse the control of hydroclimatic factors on suspended sediment concentration (SSC) in Alpine catchments by differentiating among the potential contributions of erosion and suspended sediment transport driven by erosive rainfall, defined as liquid precipitation over snow-free surfaces, ice melt from glacierized areas, and snowmelt on hillslopes. We account for the potential impact of hydropower by intercepting sediment fluxes originated in areas diverted to hydropower reservoirs, and by considering the contribution of hydropower releases to SSC. We obtain the hydroclimatic variables from daily gridded datasets of precipitation and temperature, implementing a degree-day model to simulate spatially distributed snow accumulation and snow-ice melt. We estimate hydropower releases by a conceptual approach with a unique virtual reservoir regulated on the basis of a target-volume function, representing normal reservoir operating conditions throughout a hydrological year. An Iterative Input Selection algorithm is used to identify the variables with the highest predictive power for SSC, their explained variance, and characteristic time lags. On this basis, we develop a hydroclimatic multivariate rating curve (HMRC) which accounts for the contributions of the most relevant hydroclimatic input variables mentioned above. We calibrate the HMRC with a gradient-based nonlinear optimization method and we compare its performance with a traditional discharge-based rating curve. We apply the approach in the upper Rhône Basin, a large Swiss Alpine catchment heavily regulated by hydropower. Our results show that the three hydroclimatic processes - erosive rainfall, ice melt, and snowmelt - are significant predictors of mean daily SSC, while hydropower release does not have a significant explanatory power for SSC. The characteristic time lags of the hydroclimatic variables correspond to the typical flow concentration times of the basin. Despite not including discharge, the HMRC performs better than the traditional rating curve in reproducing SSC seasonality, especially during validation at the daily scale. While erosive rainfall determines the daily variability of SSC and extremes, ice melt generates the highest SSC per unit of runoff and represents the largest contribution to total suspended sediment yield. Finally, we show that the HMRC is capable of simulating climate-driven changes in fine sediment dynamics in Alpine catchments. In fact, HMRC can reproduce the changes in SSC in the past 40 years in the Rhône Basin connected to air temperature rise, even though the simulated changes are more gradual than those observed. The approach presented in this paper, based on the analysis of the hydroclimatic control of suspended sediment concentration, allows the exploration of climate-driven changes in fine sediment dynamics in Alpine catchments. The approach can be applied to any Alpine catchment with a pluvio-glacio-nival hydrological regime and adequate hydroclimatic datasets. © 2018 Author(s).
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/163277
Appears in Collections:气候变化与战略

Files in This Item:

There are no files associated with this item.


作者单位: Costa, A., Institute of Environmental Engineering, ETH Zurich, Zurich, 8093, Switzerland; Anghileri, D., Institute of Environmental Engineering, ETH Zurich, Zurich, 8093, Switzerland; Molnar, P., Institute of Environmental Engineering, ETH Zurich, Zurich, 8093, Switzerland

Recommended Citation:
Costa A.,Anghileri D.,Molnar P.. Hydroclimatic control on suspended sediment dynamics of a regulated Alpine catchment: A conceptual approach[J]. Hydrology and Earth System Sciences,2018-01-01,22(6)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Costa A.]'s Articles
[Anghileri D.]'s Articles
[Molnar P.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Costa A.]'s Articles
[Anghileri D.]'s Articles
[Molnar P.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Costa A.]‘s Articles
[Anghileri D.]‘s Articles
[Molnar P.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.