The Himalayan rivers yield the most significant flux of continental sediments into ocean. Organic matter (OM) transported by these provides a peek at influence diverse geological terrains, soil types, vegetation, and climate on carbon cycling within narrow boundary. We analyzed suspended bedload from four to trace their sources, elucidate fate during fluvial transport, estimate organic (OC) flu...

Accurately determining sediment loads is necessary for managing river environments but difficult because multiple processes can lead to large discharge-independent changes in transport. Thus, estimations of load using discharge–sediment rating curves fit sparse or historical sediment-transport measurements be inaccurate, necessitating alternative approaches reduce uncertainty. Continuous uncert...

Bedload transport is a key process in fluvial morphodynamics, but difficult to measure. The advent of seismic monitoring techniques has provided an alternative in-stream monitoring, which often costly and cannot be utilized during large floods. Seismic method requiring several steps convert data into bedload flux data. State-of-the-art conversion approaches exploit physical models predicting th...