An Overlooked Issue of Variational Data Assimilation

被引:8
作者
Menetrier, Benjamin [1 ]
Auligne, Thomas [1 ]
机构
[1] NCAR, Mesoscale & Microscale Meteorol Lab, Boulder, CO 80301 USA
关键词
Optimization; Variational analysis; ERROR COVARIANCES; 4D-VAR; SYSTEM; NWP;
D O I
10.1175/MWR-D-14-00404.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The control variable transform ( CVT) is a keystone of variational data assimilation. In publications using such a technique, the background term of the transformed cost function is defined as a canonical inner product of the transformed control variable with itself. However, it is shown in this paper that this practical definition of the cost function is not correct if the CVT uses a square root of the background error covariance matrix B that is not square. Fortunately, it is then shown that there is a manifold of the control space for which this flaw has no impact, and that most minimizers used in practice precisely work in this manifold. It is also shown that both correct and practical transformed cost functions have the same minimum. This explains more rigorously why the CVT is working in practice. The case of a singular B is finally detailed, showing that the practical cost function still reaches the best linear unbiased estimate ( BLUE).
引用
收藏
页码:3925 / 3930
页数:6
相关论文
共 14 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]   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
[3]  
COURTIER P, 1994, Q J ROY METEOR SOC, V120, P1367, DOI 10.1256/smsqj.51911
[4]  
DERBER J, 1989, J PHYS OCEANOGR, V19, P1333, DOI 10.1175/1520-0485(1989)019<1333:AGODAS>2.0.CO
[5]  
2
[6]   Preconditioning of variational data assimilation and the use of a bi-conjugate gradient method [J].
El Akkraoui, Amal ;
Tremolet, Yannick ;
Todling, Ricardo .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2013, 139 (672) :731-741
[7]  
Fisher M., 2003, P ECMWF SEM REC DEV, P45
[8]   B-preconditioned minimization algorithms for variational data assimilation with the dual formulation [J].
Guerol, S. ;
Weaver, A. T. ;
Moore, A. M. ;
Piacentini, A. ;
Arango, H. G. ;
Gratton, S. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2014, 140 (679) :539-556
[9]   The Met. Office global three-dimensional variational data assimilation scheme [J].
Lorenc, AC ;
Ballard, SP ;
Bell, RS ;
Ingleby, NB ;
Andrews, PLF ;
Barker, DM ;
Bray, JR ;
Clayton, AM ;
Dalby, T ;
Li, D ;
Payne, TJ ;
Saunders, FW .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2000, 126 (570) :2991-3012
[10]   The potential of the ensemble Kalman filter for NWP - a comparison with 4D-Var [J].
Lorenc, AC .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2003, 129 (595) :3183-3203