Development and Application of a Large‐Scale, Physically Based, Distributed Suspended Sediment Transport Model on the Fraser River Basin, British Columbia, Canada. Issue 10 (22nd October 2018)

• Record Type: Journal Article
• Authors: Tsuruta, Kai; Hassan, Marwan A.; Donner, Simon D.; Alila, Younes
• Is Part Of: Journal of geophysical research. Volume 123:Issue 10(2018)
• Page Start: 2481
• Page End: 2508
• Publication Date: 2018-10-22
• Subjects: large‐scale modeling -- sediment transport -- Fraser River Basin; Geomorphology -- Periodicals; 551.3
• DOI: 10.1029/2017JF004578
• Languages: English
• ISSNs: 2169-9003

Abstract

Abstract : Modeling sediment transport through large basins presents a challenging problem. The relation between water flux and sediment load is complex, and substantial erosion and transport can occur over small spatial and temporal scales. Analysis of large‐scale basins often relies on lumped empirical models that do not consider spatial or subannual variability. In this study, we adapt a small‐scale, mechanistic, distributed suspended sediment transport model for application to large basins. The model is integrated into the Terrestrial Hydrology Model with Biochemistry to make use of the Terrestrial Hydrology Model with Biochemistry's dynamic water routing. The coupled model is applied to the 230, 000‐km 2 Fraser River Basin in British Columbia, Canada, using climatic and hydrological inputs provided by a historical run of the Variable Infiltration Capacity model. Hourly simulations are aggregated into monthly and long‐term averages which are compared against observations. Simulated long‐term lake sedimentation values are within an order of magnitude of observations, and monthly load simulations have an average R 2 of 0.70 across the five study stations with available data. Model results indicate that sediment loads from tributaries do not heavily influence dynamics along the main stem and suggest the importance of network connectivity. Sensitivity analysis indicates that models may benefit from characterizing bed load irrespective of its contribution to total sediment load. Historical simulations over the 1965–2004 period reveal important changes in sediment dynamics that could not be captured with a lumped model, including a decrease in basin sediment load interannual variability driven by changes in runoff and load variability within a key subbasin. Key Points: A mechanistic sediment transport routine is integrated into a hydrological model to provide river, lake, and floodplain dynamics at each grid cell across a large basin The distributed model provides insights into the basin's sediment transport that are not possible with a lumped approach Tributaries in the study area, even those in mountainous regions, do not substantially impact basin sediment yield