Climate Dynamics

, Volume 41, Issue 5–6, pp 1407–1417 | Cite as

Ocean mixed layer processes in the Pacific Decadal Oscillation in coupled general circulation models

  • Bo Young Yim
  • Yign Noh
  • Sang-Wook Yeh
  • Jong-Seong Kug
  • Hong Sik Min
  • Bo Qiu
Article

Abstract

It is investigated how the Pacific Decadal Oscillation (PDO) is simulated differently among various coupled general circulation models (CGCMs), and how it is related to the heat budget of the simulated ocean mixed layer, which includes the surface heat flux and ocean heat transport. For this purpose the dataset of the climate of the 20th Century experiment (20C3M) from nine CGCMs reported to IPCC’s AR4 are used, while the MRI and MIROC models are examined in detail. Detailed analyses of these two CGCMs reveal that the PDO is mainly affected by ocean heat transport rather than surface heat flux, in particular in the MRI model which has a larger contribution of ocean heat transport to the heat budget. It is found that the ocean heat transport due to Ekman advection versus geostrophic advection contributes differently to the PDO in the western and central North Pacific. Specifically, the strength of PDO tends to be larger for CGCMs with a larger ocean heat transport in the region.

Keywords

Pacific Decadal Oscillation El Niño and Southern Oscillation Coupled general circulation models Heat budget of the mixed layer 

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Copyright information

© Springer-Verlag Berlin Heidelberg 2012

Authors and Affiliations

  • Bo Young Yim
    • 1
  • Yign Noh
    • 2
  • Sang-Wook Yeh
    • 3
  • Jong-Seong Kug
    • 1
  • Hong Sik Min
    • 1
  • Bo Qiu
    • 4
  1. 1.Korea Institute of Ocean Science and TechnologyAnsanSouth Korea
  2. 2.Department of Atmospheric Sciences/Global Environmental LaboratoryYonsei UniversitySeoulSouth Korea
  3. 3.Department of Environmental Marine ScienceHanyang UniversityAnsanSouth Korea
  4. 4.Department of OceanographyUniversity of Hawaii at ManoaHonoluluUSA

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