4.7 Article

Understanding the key factors that influence soil moisture estimation using the unscented weighted ensemble Kalman filter

期刊

AGRICULTURAL AND FOREST METEOROLOGY
卷 313, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.agrformet.2021.108745

关键词

Soil moisture; One-dimensional vertical water flow model; Unscented weighted ensemble Kalman filter (UWEnKF); Data assimilation; Uncertainty

资金

  1. National Key R&D Program of China [2016YFC0402710]
  2. National Natural Science Foundation of China [51709046, 51539003, 41761134090, 41830752, 52109036]
  3. Special Fund of State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering [20195025612, 20195018812, 520004412]
  4. Arid Meteorology Sciences Research Foundation [IAM202119]
  5. startup funds of Yangzhou University [137012321]

向作者/读者索取更多资源

This study evaluated the effects of uncertainties in multiple factors on soil moisture estimation and demonstrated the effectiveness of the unscented weighted ensemble Kalman filter (UWEnKF) in improving soil moisture estimations in a data assimilation system.
Accurate quantification of soil moisture contributes significantly to an understanding of land surface processes. In-situ observable soil moisture data are often sparsely distributed, and model performance is influenced by many factors. In this study, 14 numerical experimental schemes about the effects of uncertainties in multiple factors (soil property, time step, assimilation interval, precipitation, soil layer thickness and initial value) on soil moisture estimation were evaluated based on the unscented weighted ensemble Kalman filter (UWEnKF) and a one-dimensional vertical water flow model at the ELBARA field site in the Maqu monitoring network in the upper reaches of the Yellow River, China. The experiments showed that soil properties had little effect on model pa-rameters (e.g., saturated soil moisture content, saturated soil hydraulic conductivity, saturated soil matric po-tential) in either the horizontal or vertical direction using the model numerical solving scheme adopted, and thus had little effect on soil moisture estimation. Using only the observed K-sat may lead to better soil moisture pre-dictions. Reducing the simulation time step has limited impact on soil moisture estimation. The effects of pre-cipitation on soil moisture estimations varied due to overestimation or underestimation of soil moisture content in different soil layers, and differences in soil layer thicknesses led to uncertainty in soil moisture estimation. The model accurately predicted the change trend of soil moisture if the initial values were reasonable. UWEnKF performed well in terms of improving soil moisture estimations despite the uncertainty of many factors in data assimilation system, and performed better with high assimilation frequency (i.e., small assimilation interval). Thus, UWEnKF is an effective and practical technique for soil moisture assimilation whatever the uncertainty of multiple factors is.

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