Ensemble Kalman Filter Data Assimilation for the Model for Prediction Across Scales (MPAS)

被引:25
|
作者
Ha, Soyoung [1 ]
Snyder, Chris [1 ]
Skamarock, William C. [1 ]
Anderson, Jeffrey [1 ]
Collins, Nancy [1 ]
机构
[1] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
基金
美国国家科学基金会;
关键词
ADAPTIVE COVARIANCE INFLATION; VARIATIONAL DATA ASSIMILATION; ERROR-CORRECTION; SYSTEM; IMPLEMENTATION; LOCALIZATION; BALANCE; SCHEME;
D O I
10.1175/MWR-D-17-0145.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A global atmospheric analysis and forecast system is constructed based on the atmospheric component of the Model for Prediction Across Scales (MPAS-A) and the Data Assimilation Research Testbed (DART) ensemble Kalman filter. The system is constructed using the unstructured MPAS-A Voronoi (nominally hexagonal) mesh and thus facilitates multiscale analysis and forecasting without the need for developing new covariance models at different scales. Cycling experiments with the assimilation of real observations show that the global ensemble system is robust and reliable throughout a one-month period for both quasi-uniform and variable-resolution meshes. The variable-mesh assimilation system consistently provides higher-quality analyses than those from the coarse uniform mesh, in addition to the benefits of the higher-resolution forecasts, which leads to substantial improvements in 5-day forecasts. Using the fractions skill score, the spatial scale for skillful precipitation forecasts is evaluated over the high-resolution area of the variable-resolution mesh. Skill decreases more rapidly at smaller scales, but the variable mesh consistently outperforms the coarse uniform mesh in precipitation forecasts at all times and thresholds. Use of incremental analysis updates (IAU) greatly decreases high-frequency noise overall and improves the quality of EnKF analyses, particularly in the tropics. Important aspects of the system design related to the unstructured Voronoi mesh are also investigated, including algorithms for handling the C-grid staggered horizontal velocities.
引用
收藏
页码:4673 / 4692
页数:20
相关论文
共 50 条
  • [31] A modified iterative ensemble Kalman filter data assimilation method
    Xu, Baoxiong
    Bai, Yulong
    Wang, Yizhao
    Li, Zhe
    Ma, Boyang
    [J]. 2ND INTERNATIONAL CONFERENCE ON MATERIALS SCIENCE, ENERGY TECHNOLOGY AND ENVIRONMENTAL ENGINEERING (MSETEE 2017), 2017, 81
  • [32] A multimodel data assimilation framework via the ensemble Kalman filter
    Xue, Liang
    Zhang, Dongxiao
    [J]. WATER RESOURCES RESEARCH, 2014, 50 (05) : 4197 - 4219
  • [33] Comment on 'Data assimilation using an ensemble kalman filter technique'
    van Leeuwen, P.J.
    [J]. Monthly Weather Review, 1999, 127 (6 1/2): : 1374 - 1377
  • [34] A suboptimal data assimilation algorithm based on the ensemble Kalman filter
    Klimova, Ekaterina
    [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2012, 138 (669) : 2079 - 2085
  • [35] Comment on `Data assimilation using a ensemble Kalman filter technique'
    van, Leeuwen, Peter Jan
    [J]. Monthly Weather Review, 127 (6 II): : 1374 - 1377
  • [36] Comment on "Data assimilation using an ensemble Kalman filter technique"
    van Leeuwen, PJ
    [J]. MONTHLY WEATHER REVIEW, 1999, 127 (06) : 1374 - 1377
  • [37] An adaptive ensemble Kalman filter for soil moisture data assimilation
    Reichle, Rolf H.
    Crow, Wade T.
    Keppenne, Christian L.
    [J]. WATER RESOURCES RESEARCH, 2008, 44 (03)
  • [38] Balanced multivariate model errors of an intermediate coupled model for ensemble Kalman filter data assimilation
    Zheng, Fei
    Zhu, Jiang
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2008, 113 (C7)
  • [39] Data assimilation in groundwater modelling: ensemble Kalman filter versus ensemble smoothers
    Li, Liangping
    Puzel, Ryan
    Davis, Arden
    [J]. HYDROLOGICAL PROCESSES, 2018, 32 (13) : 2020 - 2029
  • [40] Ensemble Kalman filter based data assimilation for tropical waves in the MJO skeleton model
    Gleiter, Tabea
    Janjic, Tijana
    Chen, Nan
    [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2022, 148 (743) : 1035 - 1056