4.7 Article

Mapping inter- and intra-annual dynamics in water surface area of the Tonle Sap Lake with Landsat time-series and water level data

期刊

JOURNAL OF HYDROLOGY
卷 601, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.jhydrol.2021.126644

关键词

Lakeshore elevation model; Landsat images; Remote sensing water indices; Hydropower development; Tonle Sap Lake

资金

  1. National Science and Technology Support Program of China [2013BAB06B03]
  2. National Natural Science Foundation of China [41971239]
  3. China Postdoctoral Science Foundation [2019M653506, 2019HC027]

向作者/读者索取更多资源

This study presents a method for water monitoring based on multi-temporal Landsat images, combined with LEM to effectively remove cloud cover effects, for long-term monitoring of Tonle Sap Lake water areas. The results show that over the past 30 years, there has been no significant change in the water area of Tonle Sap Lake.
Surface water monitoring is the foundation of water resources management. However, large-scale surface water monitoring based on long-sequence Landsat images is easily affected by cloud cover. In this study, taking the Tonle Sap Lake in the lower Mekong as an example, a series of water-land boundaries with height attributes based on water level data were extracted from multi-temporal Landsat images without cloud cover using the optimal water index and the lakeshore elevation model (LEM) of Tonle Sap Lake was constructed. On this basis, with the help of the limited land-water boundary provided by the Landsat image over a longer period, long-term monitoring of the changes in the water area of the entire lake area was realized. The results show that the Landsat image data in conjunction with the LEM can effectively remove the effect of cloud cover in monitoring the change of long time series water bodies. Reconstruction of historical data on changes in the waters of Tonle Sap Lake with the proposed method shows that in the past 30 years, there has been no significant change in the water areas of Tonle Sap Lake in either the dry or rainy seasons. Water area changes of the lake have a delayed response of 1-3 months to changes in the water level of the Mekong River, which is more affected by the mainstream recharge. The water area of the lake is unaffected in the dry season; however, it is weakly affected in the rainy season by the Xiaowan and Nuozhadu hydropower stations in China.

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