4.7 Article

Century-Scale Reconstruction of Water Storage Changes of the Largest Lake in the Inner Mongolia Plateau Using a Machine Learning Approach

期刊

WATER RESOURCES RESEARCH
卷 57, 期 2, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020WR028831

关键词

atmospheric circulation; climate change; Lake Hulun; machine learning; water storage

资金

  1. National Key Research and Development Program of China [2019YFA0607101, 2018YFD0900804, 2018YFD1100101]
  2. Thousand Young Talents Program in China [Y7QR011001]
  3. Strategic Priority Research Program of the Chinese Academy of Sciences [XDA23100102]
  4. National Natural Science Foundation of China [41971403, 41801321]

向作者/读者索取更多资源

The study aims to reconstruct the water storage changes of Lake Hulun over the past century, with results showing the highest water storage in the 1960s and the lowest point in the 1930s-1940s. The XGBoost model demonstrates effective performance in predicting century-scale water storage variations, with precipitation being the most influential factor.
Lake Hulun is the fifth-largest lake in China, playing a substantial role in maintaining the balance of the grassland ecosystem of the Mongolia Plateau, which is a crucial ecological barrier in North China. To better understand the changing characteristics of Lake Hulun and the driving mechanisms, it is necessary to investigate the water storage changes of Lake Hulun on extended timescales. The main objective of this study is to reconstruct the water storage time series of Lake Hulun over the past century. We employed a machine learning approach termed the extreme gradient boosting tree (XGBoost) to reconstruct the water storage changes over a one-century timescale based on the generated bathymetry and satellite altimetry data and investigated the relationships with hydrological and climatic variables in long term. Results show that the water storage changes from 1961 to 2019 were featured by four fluctuation phases, with the highest water storage observed in 1991 (14.02 Gt) and the lowest point in 2012 (5.18 Gt). The century-scale reconstruction result reveals that the water storage of Lake Hulun reached the highest point in the 1960s within the period of 1910-2019. The lowest stage occurred in the sub-period of the 1930s-1940s, which was even lower than the alerted shrinkage stage in 2012. The predictive model results indicate the effective performance of the XGBoost model in reconstructing century-scale water storage variations, with the mean absolute error of 0.68, normalized root mean square error of 0.11, Nash-Sutcliffe efficiency of 0.97, and correlation coefficient of 0.94. The annual fluctuations of water storage were mostly affected by precipitation, followed by vapor pressure, temperature, potential evapotranspiration, and wet day frequency. The dominating characteristics of different variables vary evidently with different sub-periods. The atmospheric circulations of the Arctic Oscillation, El Nino Southern Oscillation, Pacific Decadal Oscillation, and North Atlantic Oscillation have tight associations with the water storage variations of Lake Hulun, which change with different study periods.

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