Sub-daily soil moisture estimate using dynamic Bayesian model averaging

被引:16
作者
Chen, Yong [1 ,2 ,3 ]
Yuan, Huiling [1 ,2 ]
Yang, Yize [4 ]
Sun, Ruochen [5 ]
机构
[1] Nanjing Univ, Sch Atmospher Sci, Nanjing, Peoples R China
[2] Nanjing Univ, Minist Educ, Key Lab Mesoscale Severe Weather, Nanjing, Peoples R China
[3] Natl Ctr Atmospher Res, Res Applicat Lab, POB 3000, Boulder, CO 80307 USA
[4] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing, Peoples R China
[5] Hohai Univ, Coll Hydrol & Water Resources, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing, Peoples R China
基金
中国国家自然科学基金; 国家重点研发计划;
关键词
Soil moisture; Dynamic Bayesian model averaging; Reanalysis; Land data assimilation system; CLDAS; DATA ASSIMILATION; PRECIPITATION PRODUCTS; ENSEMBLE; DROUGHT; UNCERTAINTY; PERFORMANCE; VALIDATION; MULTIMODEL; SATELLITE; BASIN;
D O I
10.1016/j.jhydrol.2020.125445
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Accurate estimation of soil moisture (SM) from satellite products and model simulations at sub-daily timescale remains a challenge. This study proposes a general dynamic Bayesian model averaging (BMA) framework for merging sub-daily model products. Compared to the traditional BMA method, this study introduces adaptive weights (dynamically variant with time) for BMA members. Based on the previous evaluation work, a subset of model products is selected from eight model products as BMA members. The dynamic BMA experiment is performed for the surface SM (0-10 cm) model products at sub-daily (6-h) timescale in 2017 over the Yangtze-Huaihe river basin. The results are compared with the automatic SM observations (ASMOs) with unprecedented high spatial and temporal resolution (up to 7 stations within a 104 km(2) pixel; hourly). Because weather pattern and model performance change over time, the determination of an optimal training period is critical to obtain adaptive BMA weights for rapid weather regime changes. The sensitivity of training length (days) is then examined, and the optimum data length used in the BMA training period proves to be about 80 days. With deterministic and probabilistic verification metrics, the dynamic BMA estimated SM is comprehensively evaluated against the ASMOs, eight global model products, and the CMA's (China Meteorological Administration) regional Land Data Assimilation System (CLDAS) product. To better compare the probability distribution of different products, the cumulative distribution function (CDF) consistency histogram and a more objective metric consistency deviation (CD) are proposed to diagnose the consistency of two SM CDFs (e.g., the BMA estimated and the observed CDF). In terms of both the deterministic (the Kling-Gupta efficiency, correlation, system bias, and bias adjusted root-mean square error) and probabilistic verification methods (CD, QQ-plots, and reliability), the dynamic BMA estimated SM outperforms any BMA members and even the benchmark product CLDAS. This study demonstrates that the dynamic BMA framework provides a new solution for merging SM model products. The merged SM and the BMA combined probability distribution can be further used for drought monitoring and prediction.
引用
收藏
页数:14
相关论文
共 76 条
[1]   The Quest for Model Uncertainty Quantification: A Hybrid Ensemble and Variational Data Assimilation Framewor [J].
Abbaszadeh, Peyman ;
Moradkhani, Hamid ;
Daescu, Dacian N. .
WATER RESOURCES RESEARCH, 2019, 55 (03) :2407-2431
[2]   Downscaling SMAP Radiometer Soil Moisture Over the CONUS Using an Ensemble Learning Method [J].
Abbaszadeh, Peyman ;
Moradkhani, Hamid ;
Zhan, Xiwu .
WATER RESOURCES RESEARCH, 2019, 55 (01) :324-344
[3]   Soil moisture spatial variability in experimental areas of central Italy [J].
Brocca, L. ;
Morbidelli, R. ;
Melone, F. ;
Moramarco, T. .
JOURNAL OF HYDROLOGY, 2007, 333 (2-4) :356-373
[4]   Improving runoff prediction through the assimilation of the ASCAT soil moisture product [J].
Brocca, L. ;
Melone, F. ;
Moramarco, T. ;
Wagner, W. ;
Naeimi, V. ;
Bartalis, Z. ;
Hasenauer, S. .
HYDROLOGY AND EARTH SYSTEM SCIENCES, 2010, 14 (10) :1881-1893
[5]   Soil moisture estimation through ASCAT and AMSR-E sensors: An intercomparison and validation study across Europe [J].
Brocca, L. ;
Hasenauer, S. ;
Lacava, T. ;
Melone, F. ;
Moramarco, T. ;
Wagner, W. ;
Dorigo, W. ;
Matgen, P. ;
Martinez-Fernandez, J. ;
Llorens, P. ;
Latron, J. ;
Martin, C. ;
Bittelli, M. .
REMOTE SENSING OF ENVIRONMENT, 2011, 115 (12) :3390-3408
[6]   ASCAT soil wetness index validation through in situ and modeled soil moisture data in central Italy [J].
Brocca, L. ;
Melone, F. ;
Moramarco, T. ;
Wagner, W. ;
Hasenauer, S. .
REMOTE SENSING OF ENVIRONMENT, 2010, 114 (11) :2745-2755
[7]  
Chen F, 2001, MON WEATHER REV, V129, P587, DOI 10.1175/1520-0493(2001)129<0587:CAALSH>2.0.CO
[8]  
2
[9]   Evaluation of nine sub-daily soil moisture model products over China using high-resolution in situ observations [J].
Chen, Yong ;
Yuan, Huiling .
JOURNAL OF HYDROLOGY, 2020, 588
[10]   Probabilistic forecasting of seasonal droughts in the Pearl River basin, China [J].
Chen, Yongqin David ;
Zhang, Qiang ;
Xiao, Mingzhong ;
Singh, Vijay P. ;
Zhang, Sheng .
STOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENT, 2016, 30 (07) :2031-2040