A new intermediate coupled model for El Niño simulation and prediction

Rong Hua Zhang, Stephen E. Zebiak, Richard Kleeman, Noel Keenlyside

Research output: Contribution to journalArticlepeer-review

Abstract

A new intermediate coupled model (ICM) is developed and used to simulate and predict sea surface temperature (SST) variability in the tropical Pacific. The ocean component is based on an intermediate complexity model developed by Keenlyside and Kleeman [2002] that is an extension of the McCreary [1981] baroclinic modal model to include varying stratification and partial nonlinearity effects, allowing realistic simulation of the mean equatorial circulation and its variability. An empirical procedure is developed to parameterize subsurface entrainment temperature (Te) in terms of sea surface pressure (SSP) anomalies. The ocean model is then coupled to a statistical atmospheric model. The coupled system realistically produces interannual variability associated with El Niño. Hindcasts are made during the period 1980-1997 for lead times out to 12 months. Observed SST anomalies are the only field to be incorporated into the coupled system to initialize predictions. Predicted SST anomalies from this model do not show obvious systematic biases. Another striking feature is that the model skill beats persistence at all lead times over the central equatorial Pacific.

Original languageEnglish (US)
Pages (from-to)OCE 5-1 - OCE 5-4
JournalGeophysical Research Letters
Volume30
Issue number19
DOIs
StatePublished - Oct 1 2003

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'A new intermediate coupled model for El Niño simulation and prediction'. Together they form a unique fingerprint.

Cite this