El Niño and the Southern Oscillation
Multiscale Variability and Global and Regional Impacts
Edited by Henry F. Diaz
Edited by Vera Markgraf
Publisher: Cambridge University Press
Print Publication Year: 2000
Online Publication Date:August 2010
Chapter DOI: http://dx.doi.org/10.1017/CBO9780511573125.002
Efforts to improve our understanding of the various types of natural variability inherent in the global climate system have included a growing focus on interactions between the El Niño/Southern Oscillation (ENSO) phenomenon and lower frequency decadal- to secular-scale fluctuations in climate. New global historical instrumental data compilations are being analyzed by increasingly more sophisticated objective analysis techniques that are beginning to resolve important physical links and modulations involving dominant climatic signals. This chapter details the current historical observational evidence for interactions between ENSO and decadal- to secular-scale fluctuations in the climate system.
Spectral analyses of global historical sea surface temperature (SST) and mean sea level pressure (MSLP) anomalies reveal significant climatic signals at about 2–2.5,2.5–7, 11–13, 15–20, 20–30, and 60–80 years and a long-term secular trend. The spatial and temporal characteristics of the SST and MSLP signals in these bands are resolved and examined by using joint empirical orthogonal function (EOF) and singular value decomposition (SVD) analyses. The ENSO signal is seen to consist of quasi-biennial (QB) (2- to 2.5-year) and lower frequency (LF) (2.5- to 7-year) components that interact to produce important modulations of the phenomenon. However, longer duration ENSO characteristics and climatic fluctuations are the result of decadal- to secular-scale influences. Protracted El Niño and La Nina phases are found to be a consequence of the “phasing” of quasi-decadal (11- to 13-year) and interdecadal (15- to 20-year) ENSOlike signals with higher frequency QB and LF ENSO components.