Articles | Volume 26, issue 3
https://doi.org/10.5194/hess-26-665-2022
https://doi.org/10.5194/hess-26-665-2022
Research article
 | 
10 Feb 2022
Research article |  | 10 Feb 2022

A new large-scale suspended sediment model and its application over the United States

Hong-Yi Li, Zeli Tan, Hongbo Ma, Zhenduo Zhu, Guta Wakbulcho Abeshu, Senlin Zhu, Sagy Cohen, Tian Zhou, Donghui Xu, and L. Ruby Leung

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Cited articles

Abeshu, G. W., Li, H.-Y., Zhu, Z., Tan, Z., and Leung, L. R.: Median bed-material sediment particle size across rivers in the contiguous U.S., Earth Syst. Sci. Data Discuss. [preprint], https://doi.org/10.5194/essd-2021-201, in review, 2021. 
An, C., Moodie, A. J., Ma, H., Fu, X., Zhang, Y., Naito, K., and Parker, G.: Morphodynamic model of the lower Yellow River: Flux or entrainment form for sediment mass conservation?, Earth Surf. Dynam., 6, 989–1010, https://doi.org/10.5194/esurf-6-989-2018, 2018. 
An, C., Gong, Z., Naito, K., Parker, G., Hassan, M. A., Ma, H., and Fu, X.: Grain Size-Specific Engelund-Hansen Type Relation for Bed Material Load in Sand-Bed Rivers, With Application to the Mississippi River, Water Resour. Res., 57, e2020WR027517, https://doi.org/10.1029/2020WR027517, 2021. 
Berhe, A. A., Barnes, R. T., Six, J., and Marín-Spiotta, E.: Role of Soil Erosion in Biogeochemical Cycling of Essential Elements: Carbon, Nitrogen, and Phosphorus, Annu. Rev. Earth Planet. Sci., 46, 521–548, https://doi.org/10.1146/annurev-earth-082517-010018, 2018. 
Biedenharn, D. S., Hubbard, L. C., Thorne, C. R., and Watson, C. C.: Understanding sediment sources, pathways and sinks in regional sediment management: Wash load and bed-material load concept, SWWRP Technical Notes Collection, ERDC TN-SWWRP-06-3, US Army Engineer Research and Development Center, Vicksburg, MS, 2006. 
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Short summary
We introduce a new multi-process river sediment module for Earth system models. Application and validation over the contiguous US indicate a satisfactory model performance over large river systems, including those heavily regulated by reservoirs. This new sediment module enables future modeling of the transportation and transformation of carbon and nutrients carried by the fine sediment along the river–ocean continuum to close the global carbon and nutrient cycles.