ArticleScientific data2022
A bankfull geometry dataset for major exorheic rivers on the Qinghai-Tibet Plateau.
Article in Scientific data, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.
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Who cites it
4 citing papers in PubMed.
- Hydraulic geometry hypothesis allows reverse engineering of 3D quasi-equilibrium landscapes from 2D channel networks: Earth, Mars, Titan.Proceedings of the National Academy of Sciences of the United States of America · 2026Article
- Impacts of climate change and land use dynamics on soil erosion in the Qinghai-Tibet plateau.Scientific reports · 2026Article
- Recent intensified erosion and massive sediment deposition in Tibetan Plateau rivers.Nature communications · 2024Article
- A bankfull geometry dataset for major exorheic rivers on the Qinghai-Tibet Plateau.Scientific data · 2022Article
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Authors and funding
6 authors.
Funding
Abstract
Bankfull river discharge shapes river morphology. The bankfull river surface planform and river width can be used to quantify river size. Regional studies of stream ecology, hydrologic modelling, river carbon emissions and geomorphology from the perspective of fluvial processes are hindered by the lack of a highly accurate spatially distributed river network that considers bankfull river geometry. Based on Sentinel-2 and Landsat 5/7/8 multispectral instrument imagery and in situ measured hydrological data, the river discharge and width of spatially distributed cross sections of six major exorheic rivers and their tributaries located on the Qinghai-Tibet Plateau (QTP) are calculated under bankfull conditions. Then, the bankfull river surface is extracted. Finally, a bankfull river width and surface area database is established. The provided planform river hydromorphology data can supplement global hydrography datasets and effectively represent the combined fluvial geomorphology and geological background in the study area.
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