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The dynamics of suspended sediment production and transport in large rivers are essential geomorphologicalprocesses that can influence biodiversity. The aim of this work was to analyze the spatio-temporal variation of suspendedsediment transport in the lower Negro River using Sentinel-2 images. The suspended sediment concentration (SSC) wasestimated from the reflectance of band 4 of the MSI sensor onboard the Sentinel-2A and Sentinel-2B. The results indicate thatthe hydrological regime controls the temporal variability of SSC, being higher in the low water period and lower duringflooding, with a mean concentration of 5.28 mg L-1 for the period 2015–2019. Analysis of the spatial variation of SSC inSentinel-2 images indicated a zone of active sediment deposition located downstream of the islands of the AnavilhanasArchipelago. Geology, forest cover, and hydrological variability are the main factors controlling the low sediment yield of thebasin, with an estimated suspended solid flux of 5.76×106 ton∙year-1 and a specific yield of 8 ton∙km-2∙year-1. Despite the lowerquantity of images between February and April, due to high cloud cover, this study showed that Sentinel-2 images could beused to monitor the temporal and spatial dynamics of suspended sediment transport in Amazonian blackwater rivers.

Suspended sediment transport estimation in Negro River (Amazon Basin) using MSI/Sentinel-2 data