Interactive Feedback between the Tropical Pacific Decadal Oscillation and ENSO in a Coupled General Circulation Model

• DOI: 10.1175/2009jcli2782.1
• Publication Date: 2009-08-05T20:04:52Z
• Authors: Jung Choi; Soon-Il An; Boris Dewitte; William W. Hsieh
• Keywords: Sensitivity studies; Sea surface temperature; Pacific decadal oscillation; 500; 551; [SDU.STU.OC] Sciences of the Universe [physics]/Earth Sciences/Oceanography; 16. Peace & justice; 530; 01 natural sciences; 13. Climate action; 14. Life underwater; ENSO; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; Coupled models; 0105 earth and related environmental sciences

Abstract The output from a coupled general circulation model (CGCM) is used to develop evidence showing that the tropical Pacific decadal oscillation can be driven by an interaction between the El Niño–Southern Oscillation (ENSO) and the slowly varying mean background climate state. The analysis verifies that the decadal changes in the mean states are attributed largely to decadal changes in ENSO statistics through nonlinear rectification. This is seen because the time evolutions of the first principal component analysis (PCA) mode of the decadal-varying tropical Pacific SST and the thermocline depth anomalies are significantly correlated to the decadal variations of the ENSO amplitude (also skewness). Its spatial pattern resembles the residuals of the SST and thermocline depth anomalies after there is uneven compensation from El Niño and La Niña events. In addition, the stability analysis of a linearized intermediate ocean–atmosphere coupled system, for which the background mean states are specified, provides qualitatively consistent results compared to the CGCM in terms of the relationship between changes in the background mean states and the characteristics of ENSO. It is also shown from the stability analysis as well as the time integration of a nonlinear version of the intermediate coupled model that the mean SST for the high-variability ENSO decades acts to intensify the ENSO variability, while the mean thermocline depth for the same decades acts to suppress the ENSO activity. Thus, there may be an interactive feedback consisting of a positive feedback between the ENSO activity and the mean state of the SST and a negative feedback between the ENSO activity and the mean state of the thermocline depth. This feedback may lead to the tropical decadal oscillation, without the need to invoke any external mechanisms.