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

被引:74
|
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
相关论文
共 50 条
  • [1] Role of north tropical atlantic SST on the ENSO simulated using CMIP3 and CMIP5 models
    Yoo-Geun Ham
    Jong-Seong Kug
    [J]. Climate Dynamics, 2015, 45 : 3103 - 3117
  • [2] Role of north tropical atlantic SST on the ENSO simulated using CMIP3 and CMIP5 models
    Ham, Yoo-Geun
    Kug, Jong-Seong
    [J]. CLIMATE DYNAMICS, 2015, 45 (11-12) : 3103 - 3117
  • [3] A possible explanation on the changes in the spatial structure of ENSO from CMIP3 to CMIP5
    Yeh, Sang-Wook
    Ham, Yoo-Geun
    Kirtman, Ben P.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2014, 41 (01) : 140 - 145
  • [4] ENSO representation in climate models: from CMIP3 to CMIP5
    Bellenger, H.
    Guilyardi, E.
    Leloup, J.
    Lengaigne, M.
    Vialard, J.
    [J]. CLIMATE DYNAMICS, 2014, 42 (7-8) : 1999 - 2018
  • [5] ENSO representation in climate models: from CMIP3 to CMIP5
    H. Bellenger
    E. Guilyardi
    J. Leloup
    M. Lengaigne
    J. Vialard
    [J]. Climate Dynamics, 2014, 42 : 1999 - 2018
  • [6] ENSO phase-locking to the boreal winter in CMIP3 and CMIP5 models
    Yoo-Geun Ham
    Jong-Seong Kug
    [J]. Climate Dynamics, 2014, 43 : 305 - 318
  • [7] ENSO phase-locking to the boreal winter in CMIP3 and CMIP5 models
    Ham, Yoo-Geun
    Kug, Jong-Seong
    [J]. CLIMATE DYNAMICS, 2014, 43 (1-2) : 305 - 318
  • [8] An evaluation of the CMIP3 and CMIP5 simulations in their skill of simulating the spatial structure of SST variability
    Wang, Gang
    Dommenget, Dietmar
    Frauen, Claudia
    [J]. CLIMATE DYNAMICS, 2015, 44 (1-2) : 95 - 114
  • [9] An evaluation of the CMIP3 and CMIP5 simulations in their skill of simulating the spatial structure of SST variability
    Gang Wang
    Dietmar Dommenget
    Claudia Frauen
    [J]. Climate Dynamics, 2015, 44 : 95 - 114
  • [10] Assessment of future ENSO changes in a CMIP3/CMIP5 multi-model and multi-index framework
    Keupp, Luzia
    Pollinger, Felix
    Paeth, Heiko
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2017, 37 (08) : 3439 - 3451