4.7 Article

Developing remote sensing methods for monitoring water quality of alpine rivers on the Tibetan Plateau

Journal

GISCIENCE & REMOTE SENSING
Volume 59, Issue 1, Pages 1384-1405

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/15481603.2022.2116078

Keywords

Water environment model; remote sensing inversion; water environment parameters; alpine river

Funding

  1. Natural Science Foundation of China [42171463, 91547107]
  2. National Key R&D Program of China [2017YFA0604702, 2018YFA0606001]

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This study proposes a method for monitoring water quality in alpine rivers on the Tibetan Plateau using hyperspectral satellite data and field observations. Novel models are built to calculate key water quality parameters, and an integrated air-ground database is generated to capture the spatial heterogeneity of the water environment.
Water quality in alpine rivers on the Tibetan Plateau is a key indicator for eco-environment security in China, which, however, is difficult to be monitored over the plateau. In this study, several regression methods and physicals models based on hyperspectral satellite data and field observations are proposed to monitor critical water quality parameters, including water turbidity (WT), total nitrogen (TN), total phosphorus (TP), and total organic carbon (TOC) in alpine rivers. Three remote sensing and field joint observation experiments were firstly carried out in these rivers in different seasons. Then, novel statistical and semi-analytical models were built to calculate the water quality parameters in these alpine rivers using hyperspectral remote sensing data. An integrated air-ground database containing long-term water quality parameters of alpine rivers was further generated to capture the spatial heterogeneity of the water environment of these rivers by using the novel models. The results indicate that WT, TP, TN, and TOC concentrations showed clear interannual cyclical variations and seasonal variations, which reflect that the water environment has a strong seasonality and are mainly controlled by climate change in the alpine plateau.

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