Dynamical Seasonal Climate Prediction Using an Ocean-Atmosphere Coupled Climate Model Developed in Partnership between South Africa and the IRI

被引:23
作者
Beraki, Asmerom F. [1 ,2 ]
DeWitt, David G. [3 ]
Landman, Willem A. [2 ,4 ]
Olivier, Cobus [1 ,2 ]
机构
[1] South African Weather Serv, ZA-0001 Pretoria, South Africa
[2] Univ Pretoria, Dept Geog Geoinformat & Meteorol, ZA-0002 Pretoria, South Africa
[3] Columbia Univ, Int Res Inst Climate & Soc, Palisades, NY USA
[4] CSIR, ZA-0001 Pretoria, South Africa
关键词
Seasonal forecasting; Coupled models; Ensembles; Model evaluation; performance; Numerical weather prediction; forecasting; Interannual variability; GENERAL-CIRCULATION MODEL; SURFACE-TEMPERATURE; SOIL-MOISTURE; PART II; FORECASTS; RAINFALL; PREDICTABILITY; SENSITIVITY; DIPOLE; INITIALIZATION;
D O I
10.1175/JCLI-D-13-00275.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The recent increase in availability of high-performance computing (HPC) resources in South Africa allowed the development of an ocean-atmosphere coupled general circulation model (OAGCM). The ECHAM4.5-South African Weather Service (SAWS) Modular Oceanic Model version 3 (MOM3-SA) is the first OAGCM to be developed in Africa for seasonal climate prediction. This model employs an initialization strategy that is different from previous versions of the model that coupled the same atmosphere and ocean models. Evaluation of hindcasts performed with the model revealed that the OAGCM is successful in capturing the development and maturity of El Nino and La Nina episodes up to 8 months ahead. A model intercomparison also indicated that the ECHAM4.5-MOM3-SA has skill levels for the Nino-3.4 region SST comparable with other coupled models administered by international centers. Further analysis of the coupled model revealed that La Nina events are more skillfully discriminated than El Nino events. However, as is typical for OAGCM, the model skill was generally found to decay faster during the spring barrier.The analysis also showed that the coupled model has useful skill up to several-months lead time when predicting the equatorial Indian Ocean dipole (IOD) during the period spanning between the middle of austral spring and the start of the summer seasons, which reaches its peak in November. The weakness of the model in other seasons was mainly caused by the western segment of the dipole, which eventually contaminates the dipole mode index (DMI). The model is also able to forecast the anomalous upper air circulations, particularly in the equatorial belt, and surface air temperature in the Southern African region as opposed to precipitation.
引用
收藏
页码:1719 / 1741
页数:23
相关论文
共 115 条
[1]   Sensitivity of dynamical seasonal forecasts to ocean initial conditions [J].
Alves, O ;
Balmaseda, MA ;
Anderson, D ;
Stockdale, T .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2004, 130 (597) :647-667
[2]  
[Anonymous], 1982, Aust. Meteor. Mag.
[3]  
[Anonymous], 1994, 206 RES DEP, DOI DOI 10.21957/E34XWHYSW
[4]   Impact of initialization strategies and observations on seasonal forecast skill [J].
Balmaseda, M. ;
Anderson, D. .
GEOPHYSICAL RESEARCH LETTERS, 2009, 36 (01)
[5]  
Barnston AG, 1996, J CLIMATE, V9, P2660, DOI 10.1175/1520-0442(1996)009<2660:SAPOGS>2.0.CO
[6]  
2
[7]  
Beraki A., 2013, 1913112 WAT RES COMM
[8]   SENSITIVITY OF A GENERAL-CIRCULATION MODEL TO PARAMETERIZATIONS OF CLOUD-TURBULENCE INTERACTIONS IN THE ATMOSPHERIC BOUNDARY-LAYER [J].
BRINKOP, S ;
ROECKNER, E .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1995, 47 (02) :197-220
[9]   Predictability of Indian Ocean sea surface temperature using canonical correlation analysis [J].
Collins, DC ;
Reason, CJC ;
Tangang, F .
CLIMATE DYNAMICS, 2004, 22 (05) :481-497
[10]  
Colman A, 1999, INT J CLIMATOL, V19, P513, DOI 10.1002/(SICI)1097-0088(199904)19:5<513::AID-JOC370>3.0.CO