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DANG Xueya, CHANG Liang, LU Na. 2019. The impact of climatic warm-wet situation of the Tibetan Plateau on the water resources and environment in Qaidam Basin[J]. Geology in China, 46(2): 359-368. doi: 10.12029/gc20190212
Citation: DANG Xueya, CHANG Liang, LU Na. 2019. The impact of climatic warm-wet situation of the Tibetan Plateau on the water resources and environment in Qaidam Basin[J]. Geology in China, 46(2): 359-368. doi: 10.12029/gc20190212
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The impact of climatic warm-wet situation of the Tibetan Plateau on the water resources and environment in Qaidam Basin

  • 1.

    Xi'an Center of Geological Survey, CGS, Xi'an 710054, Shaanxi, China

  • 2.

    Key Laboratory for Groundwater and Ecology in Arid and Semi-arid Areas, Xi'an 710054, Shaanxi, China

  • 3.

    Shaanxi Engineering Research Center of water resources and environment, Xi'an 710054, Shaanxi, China

    • Fund Project: Supported by China Geological Survey Project (No. DD20160291)
More Information
  • Author Bio: DANG Xueya, male, born in 1967, doctor, senior engineer, majors in hydrogeology and environmental geology survey and research; E-mail: 474767944@qq.com
Received Date:  04 September 2018
Revised Date:  20 January 2019
Publish Date:  25 April 2019
    Abstract

  • Through studying the changes for meteorological factors, runoff and land cover in Golmud and Delingha in Qaidam Basin, it is found that the water resources and environment has been influenced significantly by climatic warm-wet situation in the-Tibetan Plateau. In the study area, the temperature increases significantly, the drought index decreases significantly, and the climatic warm-wet situation is significant. From 2000 to 2016, the annual average temperature increased respectively 1.7℃ and 1.3℃, annual average precipitation increased respectively 2 mm and 63 mm, annual average runoff increased respectively 240×106 and 90×106 m3, compared with 1960-1999, in Golmud and Delingha basin. From 2000 to 2012, the bare land in the whole basin decreased, the area of grassland, permanent ice, snow, water area and open shrub increased, and ecological vegetation was developed very well. The climatic warm-wet situation promotes the increase in precipitation, and it is the main reason for the increase of runoff, water resources, as well as the improvement of ecological environment. At the present stage, the warm-wet environment is beneficial to water resources development and ecological environmental protection in Qaidam Basin; nevertheless, the sustainable development of the water resources and environment needs further monitoring and deep research.

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