Initiation of ensemble data assimilation

被引:37
作者
Zupanski, M [1 ]
Fletcher, SJ
Navon, IM
Uzunoglu, B
Heikes, RP
Randall, DA
Ringler, TD
Daescu, D
机构
[1] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
[2] Florida State Univ, Dept Math, Tallahassee, FL 32306 USA
[3] Florida State Univ, Sch Computat Sci & Informat Technol, Tallahassee, FL 32306 USA
[4] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[5] Portland State Univ, Dept Math & Stat, Portland, OR 97207 USA
关键词
D O I
10.1111/j.1600-0870.2006.00173.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The specification of the initial ensemble for ensemble data assimilation is addressed. The presented work examines the impact of ensemble initiation in the Maximum Likelihood Ensemble Filter (MLEF) framework, but is also applicable to other ensemble data assimilation algorithms. Two methods are considered: the first is based on the use of the Kardar-Parisi-Zhang (KPZ) equation to form sparse random perturbations, followed by spatial smoothing to enforce desired correlation structure, while the second is based on the spatial smoothing of initially uncorrelated random perturbations. Data assimilation experiments are conducted using a global shallow-water model and simulated observations. The two proposed methods are compared to the commonly used method of uncorrelated random perturbations. The results indicate that the impact of the initial correlations in ensemble data assimilation is beneficial. The root-mean-square error rate of convergence of the data assimilation is improved, and the positive impact of initial correlations is notable throughout the data assimilation cycles. The sensitivity to the choice of the correlation length scale exists, although it is not very high. The implied computational savings and improvement of the results may be important in future realistic applications of ensemble data assimilation.
引用
收藏
页码:159 / 170
页数:12
相关论文
共 72 条
[1]   Assimilation of surface pressure observations using an ensemble filter in an idealized global atmospheric prediction system [J].
Anderson, JL ;
Wyman, B ;
Zhang, SQ ;
Hoar, T .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2005, 62 (08) :2925-2938
[2]  
Anderson JL, 2003, MON WEATHER REV, V131, P634, DOI 10.1175/1520-0493(2003)131<0634:ALLSFF>2.0.CO
[3]  
2
[4]  
Anderson JL, 2001, MON WEATHER REV, V129, P2884, DOI 10.1175/1520-0493(2001)129<2884:AEAKFF>2.0.CO
[5]  
2
[6]   NUMERICAL-SIMULATION OF THE KARDAR-PARISI-ZHANG EQUATION [J].
BECCARIA, M ;
CURCI, G .
PHYSICAL REVIEW E, 1994, 50 (06) :4560-4563
[7]  
Bishop CH, 2001, MON WEATHER REV, V129, P420, DOI 10.1175/1520-0493(2001)129<0420:ASWTET>2.0.CO
[8]  
2
[9]   A NOTE ON THE GENERATION OF RANDOM NORMAL DEVIATES [J].
BOX, GEP ;
MULLER, ME .
ANNALS OF MATHEMATICAL STATISTICS, 1958, 29 (02) :610-611
[10]   Assimilation of altimetric data in the mid-latitude oceans using the Singular Evolutive Extended Kalman filter with an eddy-resolving, primitive equation model [J].
Brasseur, P ;
Ballabrera-Poy, J ;
Verron, J .
JOURNAL OF MARINE SYSTEMS, 1999, 22 (04) :269-294