摘要
A numerical experiment of an asynchronous coupled ocean-atmosphere model has been described in this paper.A two-layer global atmosphere general circulation model(OSU/IAP-AGCM)and a two-layer North Pacific Ocean general circulation model(NPOGCM)developed by Liu et al.(1992)are used in numerical experiment.The sea surface temperature anomaly(SSTA)corresponding to the meander of the Kuroshio is treated as the initial perturbation in the Pacific Ocean and the abnormal phenomena caused by the disturbance and the interaction between atmosphere and ocean,have been studied. The numerical experiment showed that the SST anomaly in the North Pacific could induce a new 30—60 day oscillation through the coupling between atmosphere and ocean and the interaction between the meander of the Kuroshio and atmosphere circulation is a positive feedback process.
A numerical experiment of an asynchronous coupled ocean-atmosphere model has been described in this paper.A two-layer global atmosphere general circulation model(OSU/IAP-AGCM)and a two-layer North Pacific Ocean general circulation model(NPOGCM)developed by Liu et al.(1992)are used in numerical experiment.The sea surface temperature anomaly(SSTA)corresponding to the meander of the Kuroshio is treated as the initial perturbation in the Pacific Ocean and the abnormal phenomena caused by the disturbance and the interaction between atmosphere and ocean,have been studied. The numerical experiment showed that the SST anomaly in the North Pacific could induce a new 30—60 day oscillation through the coupling between atmosphere and ocean and the interaction between the meander of the Kuroshio and atmosphere circulation is a positive feedback process.
基金
The project supported by National Natural Science Foundation of China.
