Tropical Pacific Decadal Variability and Its Relation to Decadal Modulations of ENSO
- 1 October 2004
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 17 (19) , 3761-3774
- https://doi.org/10.1175/1520-0442(2004)017<3761:tpdvai>2.0.co;2
Abstract
A 1000-yr integration of a coupled ocean–atmosphere model (ECHO-G) has been analyzed to describe decadal to multidecadal variability in equatorial Pacific sea surface temperature (SST) and thermocline depth (Z20), and their relationship to decadal modulations of El Niño–Southern Oscillation (ENSO) behavior. Although the coupled model is characterized by an unrealistically regular 2-yr ENSO period, it exhibits significant modulations of ENSO amplitude on decadal to multidecadal time scales. The authors' main finding is that the structures in SST and Z20 characteristic of tropical Pacific decadal variability (TPDV) in the model are due to an asymmetry between the anomaly patterns associated with the model's El Niño and La Niña states, with this asymmetry reflecting a nonlinearity in ENSO variability. As a result, the residual (i.e., the sum) of the composite El Niño and La Niña patterns exhibits a nonzero dipole structure across the equatorial Pacific, with positive perturbation values in the east ... Abstract A 1000-yr integration of a coupled ocean–atmosphere model (ECHO-G) has been analyzed to describe decadal to multidecadal variability in equatorial Pacific sea surface temperature (SST) and thermocline depth (Z20), and their relationship to decadal modulations of El Niño–Southern Oscillation (ENSO) behavior. Although the coupled model is characterized by an unrealistically regular 2-yr ENSO period, it exhibits significant modulations of ENSO amplitude on decadal to multidecadal time scales. The authors' main finding is that the structures in SST and Z20 characteristic of tropical Pacific decadal variability (TPDV) in the model are due to an asymmetry between the anomaly patterns associated with the model's El Niño and La Niña states, with this asymmetry reflecting a nonlinearity in ENSO variability. As a result, the residual (i.e., the sum) of the composite El Niño and La Niña patterns exhibits a nonzero dipole structure across the equatorial Pacific, with positive perturbation values in the east ...Keywords
This publication has 32 references indexed in Scilit:
- On Dipolelike Variability of Sea Surface Temperature in the Tropical Indian OceanJournal of Climate, 2002
- An Orbitally Driven Tropical Source for Abrupt Climate Change*Journal of Climate, 2001
- Is El Niño Changing?Science, 2000
- The “normality” of El NiñoGeophysical Research Letters, 1999
- Interdecadal interactions between the tropics and midlatitudes in the Pacific BasinGeophysical Research Letters, 1999
- The Coupled GCM ECHO-2. Part I: The Tropical PacificMonthly Weather Review, 1997
- Interdecadal Climate Fluctuations That Depend on Exchanges Between the Tropics and ExtratropicsScience, 1997
- Secular Changes of Annual and Interannual Variability in the Tropics during the Past CenturyJournal of Climate, 1995
- Decadal-scale climate variability in the tropical and North Pacific during the 1970s and 1980s: observations and model resultsClimate Dynamics, 1994
- A Dynamic Thermodynamic Sea Ice ModelJournal of Physical Oceanography, 1979