Comparison of ensemble-based state and parameter estimation methods for soil moisture data assimilation

被引:31
作者
Chen, Weijing [1 ,2 ]
Huang, Chunlin [2 ,3 ]
Shen, Huanfeng [1 ]
Li, Xin [2 ,4 ]
机构
[1] Wuhan Univ, Sch Resource & Environm Sci, Wuhan 430079, Hubei, Peoples R China
[2] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Remote Sensing Gansu Prov, Lanzhou 730000, Gansu, Peoples R China
[3] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Heihe Remote Sensing Expt Res Stn, Lanzhou 730000, Gansu, Peoples R China
[4] Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
基金
美国国家科学基金会;
关键词
Data assimilation; Soil moisture; Brightness temperature; State-parameter estimation; Common Land Model; LAND DATA ASSIMILATION; SEQUENTIAL DATA ASSIMILATION; HYDROLOGIC DATA ASSIMILATION; SIMULATED RADAR DATA; ROOT KALMAN FILTER; MICROPHYSICAL PARAMETERS; ATMOSPHERIC STATE; SURFACE; MODEL; VEGETATION;
D O I
10.1016/j.advwatres.2015.08.003
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Model parameters are a source of uncertainty that can easily cause systematic deviation and significantly affect the accuracy of soil moisture generation in assimilation systems. This study addresses the issue of retrieving model parameters related to soil moisture via the simultaneous estimation of states and parameters based on the Common Land Model (CoLM). The state-parameter estimation algorithms AEnKF (Augmented Ensemble Kalman Filter), DEnKF (Dual Ensemble Kalman Filter) and SODA (Simultaneous optimization and data assimilation) are entirely implemented within an EnKF framework to investigate how the three algorithms can correct model parameters and improve the accuracy of soil moisture estimation. The analysis is illustrated by assimilating the surface soil moisture levels from varying observation intervals using data from Mongolian plateau sites. Furthermore, a radiation transfer model is introduced as an observation operator to analyze the influence of brightness temperature assimilation on states and parameters that are estimated at different microwave signal frequencies. Three cases were analyzed for both soil moisture and brightness temperature assimilation, focusing on the progressive incorporation of parameter uncertainty, forcing data uncertainty and model uncertainty. It has been demonstrated that EnKF is outperformed by all other methods, as it consistently maintains a bias. State-parameter estimation algorithms can provide a more accurate estimation of soil moisture than EnKF. AEnKF is the most robust method, with the lowest RMSE values for retrieving states and parameters dealing only with parameter uncertainty, but it possesses disadvantages related to increasing sources of uncertainty and decreasing numbers of observations. SODA performs well under the complex situations in which DEnKF shows slight disadvantages in terms of statistical indicators: however, the former consumes far more memory and time than the latter. (C) 2015 Elsevier Ltd. All rights reserved,
引用
收藏
页码:425 / 438
页数:14
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