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INTERDECADAL VARIABILITY IN A MODEL ATMOSPHERE
作者姓名:李发明  吴爱明
作者单位:Meteorological Station of Qingdao Airport, CAAC
摘    要:By using the simulation results of an AGCM, which had been run from 1945 to 1993 forced by COADS SST, the interdecadal variability of the model atmosphere was investigated and compared with that of NCEP reanalysis data. It was found that, interdecadal variability exists significantly in both the tropical Pacific wind fields and the mid-high latitude atmospheric circulation of the model atmosphere. The tendency of time variation and spatial distributions of the interdecadal variability of the model atmosphere are basically consistent with observation. Relative to the mid-high latitude atmospheric circulation, the simulation of tropical Pacific wind is more satisfying, which suggests that anomalous variation of SST is still the main factor for the interdecadal variability of tropical Pacific wind. It might have more significant influence on the tropical wind than on the mid-high latitude atmosphere. However, there is still obvious difference between the simulation and observation. They could be attributed to both the simulation capability of the model and absence of other factors in the model which are important for the interdecadal climate variation.

关 键 词:model  atmosphere    SST  anomalies    interdecadal  variability    mid-high  latitude  atmospheric  circulation    interdecadal  variability

INTERDECADAL VARIABILITY IN A MODEL ATMOSPHERE
LI Fa-ming and WU Ai-ming.INTERDECADAL VARIABILITY IN A MODEL ATMOSPHERE[J].Journal of Tropical Meteorology,2001,7(1):93-101.
Authors:LI Fa-ming and WU Ai-ming
Institution:1. Meteorological Station of Qingdao Airport, CAAC,
2. Institute of Oceanology, Chinese Academy of Sciences,
Abstract:By using the simulation results of an AGCM, which had been run from 1945 to 1993 forced by COADS SST, the interdecadal variability of the model atmosphere was investigated and compared with that of NCEP reanalysis data. It was found that, interdecadal variability exists significantly in both the tropical Pacific wind fields and the mid-high latitude atmospheric circulation of the model atmosphere. The tendency of time variation and spatial distributions of the interdecadal variability of the model atmosphere are basically consistent with observation. Relative to the mid-high latitude atmospheric circulation, the simulation of tropical Pacific wind is more satisfying, which suggests that anomalous variation of SST is still the main factor for the interdecadal variability of tropical Pacific wind. It might have more significant influence on the tropical wind than on the mid-high latitude atmosphere. However, there is still obvious difference between the simulation and observation. They could be attributed to both the simulation capability of the model and absence of other factors in the model which are important for the interdecadal climate variation.
Keywords:model atmosphere  SST anomalies  interdecadal variability  mid-high latitude atmospheric circulation  interdecadal variability
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