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

Authors
Yeh, Sang-WookHam, Yoo-GeunLee, June-Yi
Issue Date
Nov-2012
Publisher
American Meteorological Society
Keywords
Climate change; El Nino; Southern Oscillation
Citation
Journal of Climate, v.25, no.21, pp 7764 - 7771
Pages
8
Indexed
SCI
SCIE
SCOPUS
Journal Title
Journal of Climate
Volume
25
Number
21
Start Page
7764
End Page
7771
URI
https://scholarworks.bwise.kr/erica/handle/2021.sw.erica/31369
DOI
10.1175/JCLI-D-12-00304.1
ISSN
0894-8755
1520-0442
Abstract
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.
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ERICA 공학대학 (ERICA 해양융합공학과)
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