Climate variability and predictability associated with the Indo-Pacific Oceanic Channel Dynamics in the CCSM4 Coupled System Model

Dongliang Yuan; Peng Xu; Tengfei Xu

doi:10.1007/s00343-016-5178-y

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Climate variability and predictability associated with the Indo-Pacific Oceanic Channel Dynamics in the CCSM4 Coupled System Model

Updated：2023-05-16

- Climate variability and predictability associated with the Indo-Pacific Oceanic Channel Dynamics in the CCSM4 Coupled System Model
- Journal of Oceanology and Limnology Vol. 35, Issue 1, Pages: 23-38(2017)
- Affiliations：
  
  1. Key Laboratory of Ocean Circulation and Waves (KLOCAW) Institute of Oceanology Chinese Academy of Sciences
  2. Qingdao Collaborative Innovation Center of Marine Science and Technology
  3. University of Chinese Academy of Sciences
  4. First Institute of Oceanography State Oceanic Administration
- Author bio：
- Funds：
- DOI：10.1007/s00343-016-5178-y
  CLC：
- Online First：17 March 2016，
  
  Published：2017
- Accepted：
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Yuan, D., Xu, P. & Xu, T. Climate variability and predictability associated with the Indo-Pacific Oceanic Channel Dynamics in the CCSM4 Coupled System Model., Chin. J. Ocean. Limnol. 35, 23–38 (2017). https://doi.org/10.1007/s00343-016-5178-y
DOI：

Yuan, D., Xu, P. & Xu, T. Climate variability and predictability associated with the Indo-Pacific Oceanic Channel Dynamics in the CCSM4 Coupled System Model., Chin. J. Ocean. Limnol. 35, 23–38 (2017). https://doi.org/10.1007/s00343-016-5178-y DOI：

摘要

Abstract

An experiment using the Community Climate System Model (CCSM4)

a participant of the Coupled Model Intercomparison Project phase-5 (CMIP5)

is analyzed to assess the skills of this model in simulating and predicting the climate variabilities associated with the oceanic channel dynamics across the Indo-Pacific Oceans. The results of these analyses suggest that the model is able to reproduce the observed lag correlation between the oceanic anomalies in the southeastern tropical Indian Ocean and those in the cold tongue in the eastern equatorial Pacific Ocean at a time lag of 1 year. This success may be largely attributed to the successful simulation of the interannual variations of the Indonesian Throughflow

which carries the anomalies of the Indian Ocean Dipole (IOD) into the western equatorial Pacific Ocean to produce subsurface temperature anomalies

which in turn propagate to the eastern equatorial Pacific to generate ENSO. This connection is termed the “oceanic channel dynamics” and is shown to be consistent with the observational analyses. However

the model simulates a weaker connection between the IOD and the interannual variability of the Indonesian Throughflow transport than found in the observations. In addition

the model overestimates the westerly wind anomalies in the western-central equatorial Pacific in the year following the IOD

which forces unrealistic upwelling Rossby waves in the western equatorial Pacific and downwelling Kelvin waves in the east. This assessment suggests that the CCSM4 coupled climate system has underestimated the oceanic channel dynamics and overestimated the atmospheric bridge processes.

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Keywords

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