4.7 Article

Predicting root zone soil moisture using observations at 2121 sites across China

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 847, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2022.157425

关键词

Exponential filter method; Root zone soil moisture; Random forest classifier; China

资金

  1. National Science Foundation of China [42071327, 41671354]
  2. CAS Pioneer Hundred Talent Program, IGSNRR Supporting Fund [YJRCPT2019-101]
  3. Science for a Better Development of Inner Mongolia Program of the Bureau of Science and Technology of the Inner Mongolia Province [KJXMEEDS-2020005]

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This study estimates the root zone soil moisture (RZSM) across China using an exponential filter method and a randomforest regionalization approach. The results show that the method performs well in predicting RZSM in different soil layers, and the T parameter is controlled by climate regimes.
Root zone soil moisture (RZSM) is particularly useful for understanding hydrological processes, plant-land-atmosphere exchanges, and agriculture- and climate-related research. This study aims to estimate RZSM across China by using a one-parameter (T) exponential filter method (EF method) together with a randomforest (RF) regionalization approach and by using a large dataset containing in situ observations collected at 2121 sites across China. First, at each site, T is optimized at each of four soil layers (10-20 cm, 20-30 cm, 30-40 cm and 40-50 cm) by using 0-10-cm soil layer observations and the corresponding calibration layers. Second, an RF classifier is built for each layer according to the calibrated T values and 14 soil, climate and vegetation parameters across 2121 sites. Third, the calibrated T at each soil layer is regionalized with an established RF classifier. Spatial T maps are given for each soil layer across China. Our results show that the EF method performs reasonably well in predicting RZSM at the 10-20-cm, 20-30-cm, 30-40-cm and 40-50-cm layers, with Nash-Sutcliffe efficiency (NSE) medians of 0.73, 0.52, 0.38 and 0.27, respectively, between the observations and estimations. The T parameter shows a spatial pattern in each soil layer and is largely controlled by climate regimes. This study offers an improved RZSM estimation method using a large dataset containing in situ observations; the proposed method also has the potential to be used in other parts of the world.

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