The eastern-and central-Pacific El Ni(n)o-Southem Oscillation (EP-and CP-ENSO) have been found to be dominant in the tropical Pacific Ocean,and are characterized by interannual and decadal oscillation,respectively...The eastern-and central-Pacific El Ni(n)o-Southem Oscillation (EP-and CP-ENSO) have been found to be dominant in the tropical Pacific Ocean,and are characterized by interannual and decadal oscillation,respectively.In the present study,we defined the EP-and CP-ENSO modes by singular value decomposition (SVD) between SST and sea level pressure (SLP) anomalous fields.We evaluated the natural features of these two types of ENSO modes as simulated by the pre-industrial control runs of 20 models involved in phase five of the Coupled Model Intercomparison Project (CMIP5).The results suggested that all the models show good skill in simulating the SST and SLP anomaly dipolar structures for the EP-ENSO mode,but only 12 exhibit good performance in simulating the tripolar CP-ENSO modes.Wavelet analysis suggested that the ensemble principal components in these 12 models exhibit an interannual and multi-decadal oscillation related to the EP-and CP-ENSO,respectively.Since there are no changes in external forcing in the pre-industrial control runs,such a result implies that the decadal oscillation of CP-ENSO is possibly a result of natural climate variability rather than external forcing.展开更多
基金jointly supported by the National Natural Science Foundation of China (Grant Nos. 41221064, 41376020, 41376025, and 90711003)the key program of 2012Z001 and 2013Z002 in the Chinese Academy of Meteorological Science+1 种基金the "Strategic Priority Research Program–Climate Change: Carbon Budget and Relevant Issues" of the Chinese Academy of Sciences (Grant No. XDA05090400)supported by the Jiangsu Collaborative Innovation Center for Climate Change
文摘The eastern-and central-Pacific El Ni(n)o-Southem Oscillation (EP-and CP-ENSO) have been found to be dominant in the tropical Pacific Ocean,and are characterized by interannual and decadal oscillation,respectively.In the present study,we defined the EP-and CP-ENSO modes by singular value decomposition (SVD) between SST and sea level pressure (SLP) anomalous fields.We evaluated the natural features of these two types of ENSO modes as simulated by the pre-industrial control runs of 20 models involved in phase five of the Coupled Model Intercomparison Project (CMIP5).The results suggested that all the models show good skill in simulating the SST and SLP anomaly dipolar structures for the EP-ENSO mode,but only 12 exhibit good performance in simulating the tripolar CP-ENSO modes.Wavelet analysis suggested that the ensemble principal components in these 12 models exhibit an interannual and multi-decadal oscillation related to the EP-and CP-ENSO,respectively.Since there are no changes in external forcing in the pre-industrial control runs,such a result implies that the decadal oscillation of CP-ENSO is possibly a result of natural climate variability rather than external forcing.