Predicting root zone soil moisture with soil properties and satellite near-surface moisture data across the conterminous United States

被引:63
|
作者
Baldwin, D. [1 ,2 ]
Manfreda, S. [3 ]
Keller, K. [4 ,5 ,6 ]
Smithwick, E. A. H. [1 ,2 ,6 ]
机构
[1] Penn State Univ, Dept Geog, University Pk, PA 16802 USA
[2] Penn State Univ, Intercollegiate Grad Degree Program Ecol, University Pk, PA 16802 USA
[3] Univ Basilicata, Dept European & Mediterranean Cultures Architectu, Matera, Italy
[4] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA
[5] Carnegie Mellon Univ, Dept Engn & Publ Policy, Pittsburgh, PA 15213 USA
[6] Penn State Univ, Earth & Environm Syst Inst, University Pk, PA 16802 USA
关键词
Root; Soil; Moisture; Kalman; Advanced Microwave Scanning Radiometer; Monte Carlo Markov Chain; DATA ASSIMILATION; WATER-BALANCE; MODEL; VEGETATION; ASCAT;
D O I
10.1016/j.jhydrol.2017.01.020
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Satellite-based near-surface (0-2cm) soil moisture estimates have global coverage, but do not capture variations of soil moisture in the root zone (up to 100 cm depth) and may be biased with respect to ground-based soil moisture measurements. Here, we present an ensemble Kalman filter (EnKF) hydrologic data assimilation system that predicts bias in satellite soil moisture data to support the physically based Soil Moisture Analytical Relationship (SMAR) infiltration model, which estimates root zone soil moisture with satellite soil moisture data. The SMAR-EnKF model estimates a regional-scale bias parameter using available in situ data. The regional bias parameter is added to satellite soil moisture retrievals before their use in the SMAR model, and the bias parameter is updated continuously over time with the EnKF algorithm. In this study, the SMAR-EnKF assimilates in situ soil moisture at 43 Soil Climate Analysis Network (SCAN) monitoring locations across the conterminous U.S. Multivariate regression models are developed to estimate SMAR parameters using soil physical properties and the moderate resolution imaging spectroradiometer (MODIS) evapotranspiration data product as covariates. SMAR-EnKF root zone soil moisture predictions are in relatively close agreement with in situ observations when using optimal model parameters, with root mean square errors averaging 0.051 [cm(3) cm(-3)] (standard error, s.e. = 0.005). The average root mean square error associated with a 20-fold cross-validation analysis with permuted SMAR parameter regression models increases moderately (0.082 [cm(3) cm(-3)], s.e. =.0.004). The expected regional-scale satellite correction bias is negative in four out of six ecoregions studied (mean = -0.12 [-], s.e. = 0.002), excluding the Great Plains and Eastern Temperate Forests (0.053 [-1], s.e. = 0.001). With its capability of estimating regional-scale satellite bias, the SMAR-EnKF system can predict root zone soil moisture over broad extents and has applications in drought predictions and other operational hydrologic modeling purposes. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:393 / 404
页数:12
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