AUTHOR=Sirisena T. A. J. G. , Bamunawala Janaka , Maskey Shreedhar , Ranasinghe Roshanka 

TITLE=Comparison of process-based and lumped parameter models for projecting future changes in fluvial sediment supply to the coast

JOURNAL=Frontiers in Earth Science

VOLUME=Volume 10 - 2022

YEAR=2023

URL=https://www.frontiersin.org/journals/earth-science/articles/10.3389/feart.2022.978109

DOI=10.3389/feart.2022.978109

ISSN=2296-6463

ABSTRACT=Fluvial sediment supply is one of the primary sources of sediment received by coasts. Any significant change in sediment supply to the coast will disturb its equilibrium state. Therefore, a robust assessment of future changes in FSS is required to understand the coastal system’s status under plausible climatic variations and human activities. Here, we investigate two modelling approaches to estimate the FSS at two spatially heterogeneous river basins: the Irrawaddy River Basin (IRB), Myanmar and the Kalu River Basin (KRB), Sri Lanka. We compare the FSS obtained from a process-based model (i.e., Soil Water Assessment Tool: SWAT) and an empirical model (i.e., the BQART model) for mid- (2046-2065) and end-century (2081-2100) periods under climate change and human activities (viz, planned reservoirs considered here). Our results show that SWAT simulations project a higher sediment load compared to BQART in the IRB and vice versa in KRB (for both future periods considered). SWAT projects higher percentage changes for both future periods (relative to baseline) compared BQART projections in both basins with climate change alone (i.e., no reservoirs) and vice versa when planned reservoirs are considered. The difference between the two model projections (from SWAT and BQART) is higher in KRB, and it may imply that BQART model projections are more in line with SWAT projections at larger basins (like the IRB) than smaller basins (such as the KRB). The results of this study indicate that lumped empirical models such as BQART may be more suitable for assessing sediment yield in large basins than in small basins.