A weak-constraint 4DEnsembleVar. Part I: formulation and simple model experiments

被引:15
作者
Amezcua, Javier [1 ,2 ]
Goodliff, Michael [1 ]
Van Leeuwen, Peter Jan [1 ,2 ]
机构
[1] Univ Reading, Dept Meteorol, Reading, Berks, England
[2] Natl Ctr Earth Observat, Reading, Berks, England
来源
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY | 2017年 / 69卷
基金
欧洲研究理事会;
关键词
hybrid data assimilation; ensemble-variational methods; model error; TRANSFORM KALMAN FILTER; DATA ASSIMILATION; METEOROLOGICAL OBSERVATIONS; THEORETICAL ASPECTS; ENSEMBLE; NWP; 4D-VAR; SYSTEM; FLOW;
D O I
10.1080/16000870.2016.1271564
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
4DEnsembleVar is a hybrid data assimilation method which purpose is not only to use ensemble flow-dependent covariance information in a variational setting, but to altogether avoid the computation of tangent linear and adjoint models. This formulation has been explored in the context of perfect models. In this setting, all information from observations has to be brought back to the start of the assimilation window using the space-time covariances of the ensemble. In large models, localisation of these covariances is essential, but the standard time-independent localisation leads to serious problems when advection is strong. This is because observation information is advected out of the localisation area, having no influence on the update. This is part I of a two-part paper in which we develop a weak-constraint formulation in which updates are allowed at observational times. This partially alleviates the time-localisation problem. Furthermore, we provide-for the first time-a detailed description of strong-and weak-constraint 4DEnVar, including implementation details for the incremental form. The merits of our new weak-constraint formulation are illustrated using the Korteweg-de-Vries equation (propagation of a soliton). The second part of this paper deals with experiments in larger and more complicated models, namely the Lorenz (1996) model and a shallow water equations model with simulated convection.
引用
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页数:17
相关论文
共 44 条
[1]   A review of forecast error covariance statistics in atmospheric variational data assimilation. II: Modelling the forecast error covariance statistics [J].
Bannister, R. N. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2008, 134 (637) :1971-1996
[2]  
Bishop CH, 2001, MON WEATHER REV, V129, P420, DOI 10.1175/1520-0493(2001)129<0420:ASWTET>2.0.CO
[3]  
2
[4]  
Bloom SC, 1996, MON WEATHER REV, V124, P1256, DOI 10.1175/1520-0493(1996)124<1256:DAUIAU>2.0.CO
[5]  
2
[6]   On the use of EDA background error variances in the ECMWF 4D-Var [J].
Bonavita, Massimo ;
Isaksen, Lars ;
Holm, Elias .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2012, 138 (667) :1540-1559
[7]   Ensemble-derived stationary and flow-dependent background-error covariances: Evaluation in a quasi-operational NWP setting [J].
Buehner, M .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2005, 131 (607) :1013-1043
[8]   Operational implementation of a hybrid ensemble/4D-Var global data assimilation system at the Met Office [J].
Clayton, A. M. ;
Lorenc, A. C. ;
Barker, D. M. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2013, 139 (675) :1445-1461
[9]  
Evensen G, 2000, MON WEATHER REV, V128, P1852, DOI 10.1175/1520-0493(2000)128<1852:AEKSFN>2.0.CO
[10]  
2