Original vegetation condition and precipitation growth rate bifurcate sediment flux trend on the Qinghai-Tibet Plateau
Abstract Riverine sediment flux on the Qinghai-Tibet Plateau follows separate trends in different headwater basins because of complicated pathways under global warming. Here we successfully reconstructed historical sediment fluxes from seven pathways at 25 hydrological stations during 1982 ~ 2022 us...
| Autors principals: | , , , , , , , , , , |
|---|---|
| Format: | Article |
| Idioma: | English |
| Publicat: |
Nature Portfolio
2025-02-01
|
| Col·lecció: | Communications Earth & Environment |
| Accés en línia: | https://doi.org/10.1038/s43247-025-02075-w |