Variation of alpine lakes from 1986 to 2019 in the Headwater Area of the Yellow River, Tibetan Plateau using Google Earth Engine

• Published in: Advances in climate change research Vol. 11; no. 1; pp. 11 - 21
• Main Authors: LUO, Dong-Liang, JIN, Hui-Jun, DU, He-Qiang, LI, Chao, MA, Qiang, DUAN, Shui-Qiang, LI, Guo-Shuai
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.03.2020; KeAi Communications Co., Ltd
• Subjects: Climate change; Google Earth Engine; Headwater Area of the Yellow River; Lake ice phenology; Lake surface area; Permafrost degradation; Headwater Area of the Yellow River; Climate change; Lake surface area; Google Earth Engine; Lake ice phenology; Permafrost degradation
• ISSN: 1674-9278; 1674-9278
• DOI: 10.1016/j.accre.2020.05.007

To understand the variations in surface water associated with changes in air temperature, precipitation, and permafrost in the Headwater Area of the Yellow River (HAYR), we studied the dynamics of alpine lakes larger than 0.01 km2 during 1986–2019 using Google Earth Engine (GEE) platform. The surface areas of water bodies in the HAYR were processed using mass remote sensing images consisting of Landsat TM/ETM+/OLI, Sentinel-2A, and MODIS based on automatic extraction of water indices under GEE. Besides, the lake ice phenology of the Sister Lakes (the Gyaring Lake and the Ngöring Lake) was derived by threshold segmenting of water/ice area ratio. Results demonstrate that the change of surface areas experienced four stages: decreasing during 1986–2004, increasing during 2004–2012, decreasing again during 2012–2017, and increasing again during 2017–2019. Correspondingly, the number of small lakes decreased (−26.5 per year), increased (139.5 per year), again decreased (−109.0 per year), and again increased (433.0 per year). Eight lakes larger than 1 km2 disappeared in 2004 but restored afterward. The overall trends in the area of small lakes (0.01–1 km2), large lakes (>1 km2), and all lakes during 1986–2019 were 0.4, 3.1, and 3.4 km2 per year, respectively. Although the onsets of freezing, freeze-up, breaking and the break-up of the Sister Lakes varied from year to year, there is no obvious trend regarding the lake ice phenology. Tendencies of lake variations in the HAYR are primarily related to the increased net precipitation and the declined aridity, followed by the construction of hydropower station around the outlet of the Ngöring Lake, as well as permafrost degradation.