Assimilating host model information into a limited area model

被引:29
作者
Dahlgren, Per [1 ]
Gustafsson, Nils [1 ]
机构
[1] Swedish Meteorol & Hydrol Inst, S-60176 Norrkoping, Sweden
关键词
data-assimilation; large-scale constraint; error covariances; limited area; host model; VARIATIONAL DATA ASSIMILATION; FORMULATION;
D O I
10.3402/tellusa.v64i0.15836
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We propose to add an extra source of information to the data-assimilation of the regional HIgh Resolution Limited Area Model (HIRLAM) model, constraining larger scales to the host model providing the lateral boundary conditions. An extra term, J(k), measuring the distance to the large-scale vorticity of the host model, is added to the cost-function of the variational data-assimilation. Vorticity is chosen because it is a good representative of the large-scale flow and because vorticity is a basic control variable of the HIRLAM variational data-assimilation. Furthermore, by choosing only vorticity, the remaining model variables, divergence, temperature, surface pressure and specific humidity will be allowed to adapt to the modified vorticity field in accordance with the internal balance constraints of the regional model. The error characteristics of the J(k) term are described by the horizontal spectral densities and the vertical eigenmodes (eigenvectors and eigenvalues) of the host model vorticity forecast error fields, expressed in the regional model geometry. The vorticity field, provided by the European Centre for Medium-range Weather Forecasts (ECMWF) operational model, was assimilated into the HIRLAM model during an experiment period of 33 d in winter with positive impact on forecast verification statistics for upper air variables and mean sea level pressure.
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页数:17
相关论文
共 9 条
[1]  
Berre L, 2000, MON WEATHER REV, V128, P644, DOI 10.1175/1520-0493(2000)128<0644:EOSAMF>2.0.CO
[2]  
2
[3]   Introducing the coupling information in a limited-area variational assimilation [J].
Guidard, Vincent ;
Fischer, Claude .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2008, 134 (632) :723-735
[4]   Three-dimensional variational data assimilation for a limited area model Part I:: General formulation and the background error constraint [J].
Gustafsson, N ;
Berre, L ;
Hörnquist, S ;
Huang, XY ;
Lindskog, M ;
Navascués, B ;
Mogensen, KS ;
Thorsteinsson, S .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2001, 53 (04) :425-446
[5]  
Gustafsson N., 2006, HIRLAM NEWSLETT, V51
[6]  
HAUGEN JE, 1993, MON WEATHER REV, V121, P2618, DOI 10.1175/1520-0493(1993)121<2618:ASLAMF>2.0.CO
[7]  
2
[8]  
HUANG X, 2002, 57 HIRLAM
[9]   Three-dimensional variational data assimilation for a limited area model Part II:: Observation handling and assimilation experiments [J].
Lindskog, M ;
Gustafsson, N ;
Navascués, B ;
Mogensen, KS ;
Huang, XY ;
Yang, X ;
Andræ, U ;
Berre, L ;
Thorsteinsson, S ;
Rantakokko, J .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2001, 53 (04) :447-468