Climate Dynamics

, Volume 12, Issue 10, pp 667–683

Interannual and interdecadal variabilities in the Pacific in an MRI coupled GCM

  • S. Yukimoto
  • M. Endoh
  • Y. Kitamura
  • A. Kitoh
  • T. Motoi
  • A. Noda
  • T. Tokioka

DOI: 10.1007/s003820050135

Cite this article as:
Yukimoto, S., Endoh, M., Kitamura, Y. et al. Climate Dynamics (1996) 12: 667. doi:10.1007/s003820050135

Abstract.

Interannual and interdecadal variabilities in the Pacific are investigated with a coupled atmosphere-ocean GCM developed at MRI, Japan. The model is run for 70 years with flux adjustments. The model shows interannual variability in the tropical Pacific which has several typical characteristics shared with the observed ENSO. A basin-scale feature of the principal SST variation for the ENSO time scale shows negative correlation in the central North Pacific with the tropical SST, similar to that of the observed one. Associated variation of the model atmosphere indicates an intensification of the Aleutian Low and a PNA-like teleconnection pattern as a response to the tropical warm SST anomaly. The ENSO time scale variability in the midlatitude ocean consists of the westward propagation of the subsurface temperature signal and the temperature variation within the shallow mixed layer forced by the anomalous atmospheric heat fluxes. For the interdecadal time scale, variation of the SST is simulated realistically with a geographical pattern similar to that for the ENSO time scale, but it has a larger relative amplitude in the northern Pacific. For the atmosphere, spatial structure of the variation in the interdecadal time scale is also similar to that in the ENSO time scale, but has smaller amplitude in the northern Pacific. Long oceanic spin-up time (>∼10 y) in the mid-high latitude, however, makes oceanic response in the interdecadal time scale larger than that in the ENSO time scale. The lagged-regression analysis for the ocean temperature variation relative to the wind stress variation indicates that interdecadal variation of the ocean subsurface at the mid-high latitudes is considered as enhanced ocean gyre spin-up process in response to the atmospheric circulation change at the mid-high latitudes, remotely forced by the interdecadal variation of the tropical SST.

Copyright information

© Springer-Verlag Berlin Heidelberg 1996

Authors and Affiliations

  • S. Yukimoto
    • 1
  • M. Endoh
    • 1
  • Y. Kitamura
    • 1
  • A. Kitoh
    • 1
  • T. Motoi
    • 1
  • A. Noda
    • 1
  • T. Tokioka
    • 2
  1. 1. Meteorological Research Institute, 1-1 Nagamine, Tsukuba, Ibaraki 305, JapanJP
  2. 2. Japan Meteorological Agency, Tokyo 100, JapanJP

Personalised recommendations