Changes in the Tropical Pacific SST Trend from CMIP3 to CMIP5 and Its Implication of ENSO

被引:77
作者
Yeh, Sang-Wook [3 ]
Ham, Yoo-Geun [1 ,2 ]
Lee, June-Yi [4 ,5 ]
机构
[1] NASA, Goddard Space Flight Ctr, Global Modeling & Assimilat Off, Greenbelt, MD 20771 USA
[2] Univ Space Res Assoc, Goddard Earth Sci Technol & Res Studies & Investi, Columbia, MD USA
[3] Hanyang Univ, Dept Environm Marine Sci, Ansan, South Korea
[4] Univ Hawaii Manoa, Dept Meteorol, Honolulu, HI 96822 USA
[5] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA
关键词
EL-NINO-LIKE; DECADAL VARIABILITY; OSCILLATION; AMPLITUDE; MODULATIONS; OCEAN;
D O I
10.1175/JCLI-D-12-00304.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study assesses the changes in the tropical Pacific Ocean sea surface temperature (SST) trend and ENSO amplitude by comparing a historical run of the World Climate Research Programme Coupled Model Intercomparison Project (CMIP) phase-5 multimodel ensemble dataset (CMIP5) and the CMIP phase-3 dataset (CMIP3). The results indicate that the magnitude of the SST trend in the tropical Pacific basin has been significantly reduced from CMIP3 to CMIP5, which may be associated with the overestimation of the response to natural forcing and aerosols by including Earth system models in CMIP5. Moreover, the patterns of tropical warming over the second half of the twentieth century have changed from a La Nina-like structure in CMIP3 to an El Nino-like structure in CMIP5. Further analysis indicates that such changes in the background state of the tropical Pacific and an increase in the sensitivity of the atmospheric response to the SST changes in the eastern tropical Pacific have influenced the ENSO properties. In particular, the ratio of the SST anomaly variance in the eastern and western tropical Pacific increased from CMIP3 to CMIP5, indicating that a center of action associated with the ENSO amplitude has shifted to the east.
引用
收藏
页码:7764 / 7771
页数:8
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