4.7 Article

Pattern of Turbidity Change in the Middle Reaches of the Yarlung Zangbo River, Southern Tibetan Plateau, from 2007 to 2017

期刊

REMOTE SENSING
卷 13, 期 2, 页码 -

出版社

MDPI
DOI: 10.3390/rs13020182

关键词

multispectral remote sensing; turbidity; Yarlung Zangbo River; S-curve model; spatial and temporal variations

资金

  1. Summer Graduate Research Assistantship at the University of Tennessee
  2. University of Tennessee's Open Publishing Support Fund

向作者/读者索取更多资源

The study utilized remote sensing technology and field measurements to analyze turbidity changes in the middle reaches of the Yarlung Zangbo River on the Tibetan Plateau, revealing an overall decreasing trend and seasonal variations. The research shows that turbidity is influenced by the confluence of tributaries, precipitation, and vegetation changes.
Turbidity is an important indicator of riverine conditions, especially in a fragile environment such as the Tibetan Plateau. Remote sensing, with the advantages of large-scale observations, has been widely applied to monitor turbidity change in lakes and rivers; however, few studies have focused on turbidity change of rivers on the Tibetan Plateau. We investigated the pattern of turbidity change in the middle reaches of the Yarlung Zangbo River, southern Tibetan Plateau, based on multispectral satellite imagery and in situ measurements. We developed empirical models from in situ measured water leaving reflectance and turbidity, and applied the best performed s-curve models on satellite imagery from Sentinel-2, Landsat 8, and Landsat 5 to derive turbidity change in 2007-2017. Our results revealed an overall decreasing spatial trend from the upper to lower streams. Seasonal variations were observed with high turbidity from July to September and low turbidity from October to May. Annual turbidity showed a temporally slightly declining trend from 2007 to 2017. The pattern of turbidity change is affected by the confluence of tributaries and the changes in precipitation and vegetation along the river. These findings provide important insights into the responses of riverine turbidity to climate and environmental changes on the Tibetan Plateau.

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