Changes of inundation area and water turbidity of Tonle Sap Lake
Responses to climate changes or upstream dam construction
Datos Bibliográficos
| ID | 15547148 |
|---|---|
| Autores | Ye Wang (0000-0001-5127-4245, Southern University of Science and Technology), Lian Feng (0000-0002-4590-3022, Southern University of Science and Technology, autor de correspondencia), Junguo Liu (0000-0002-5745-6311, Southern University of Science and Technology), Xuejiao Hou (0000-0002-1926-6074, Southern University of Science and Technology), Deliang Chen (0000-0003-0288-5618, University of Gothenburg) |
| Año | 2020 |
| Volumen | 15 |
| Número | 9 |
| Páginas | 0940a1-0940a1 |
| Fecha de publicación | 2020-08-05 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Environmental Research Letters (JOURNAL) |
| Identificadores de la revista | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Editorial | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/abac79 |
| OpenAlex | W3046974934 |
| Idioma | EN |
| Citas recibidas | 3 |
| Referencias citadas | 56 |
Using long-term Moderate Resolution Imaging Spectroradiometer (MODIS) and Landsat satellite observations, the inundation changes of Tonle Sap Lake between 1988 and 2018 were investigated. The results show that the inundation area was stable before 2000, followed by a significant shrinking trend between 2000 and 2018. Quantitative remote sensing retrievals for concentrations of the total suspended sediments (TSS) also demonstrate an evident increasing trend (7.92 mg l −1 yr −1 ) since 2000. A strong correlation (R 2 = 0.67) was found between the annual mean inundation area and concurrent precipitation in a region located in the lower basin of the Mekong River (mostly outside the drainage basin of Tonle Sap Lake). A multiple general linear model (GLM) regression further pointed to the precipitation variation as a major contributor (76.1%) to the interannual fluctuation of the inundation area, while the dams constructed in China only contributed to 6.9%. The limited impacts of Chinese dams on the inundation area of the lake could be revealed through the limited fraction of water discharge from the Mekong River within China (∼17%). The analysis also found significant impacts of inundation changes on the recent lake turbidity increase in the dry seasons. We clearly revealed that the contribution of dam construction in China to the recent lake shrinkage was insignificant when compared with the impacts of the precipitation decrease. The results of this study provide important scientific evidence for settling water volume-related transboundary disputes regarding the control of the inundation area and water turbidity of Tonle Sap Lake
Drainage basin · Geography · Hydrology (agriculture · Moderate-resolution imaging spectroradiometer · Precipitation · Satellite · Structural basin · Turbidity · Environmental Science · Flood Risk Assessment and Management · Groundwater and Watershed Analysis · Hydrology and Watershed Management Studies · Geology · Oceanography
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Scenarios for Global Biodiversity in the 21st Century
Reassessing the projections of the World Water Development Report
The impacts of climate change on water resources and agriculture in China
Global Consequences of Land Use
Recent declines in China’s largest freshwater lake
Observed changes in the water flow at Chiang Saen in the lower Mekong
River bank instability from unsustainable sand mining in the lower Mekong River
Understanding the impact of hydropower developments in the context of upstream–downstream relations in the Mekong river basin
Natural resources management for human security in Cambodia’s Tonle Sap Biosphere Reserve
Dams on the Mekong River
Impact of the Mekong River Flow Alteration on the Tonle Sap Flood Pulse
Sediment
| Obras citantes distintas | 3 |
|---|---|
| Citas por año | 0,6 |
| Intervalo de citas | 2021 - 2025 (5) |
| Velocidad de citación | recent |
| Altamente citado | No |
| Tipos de cita | Neutras: 3 |