Abstract
The evolution of the Southern Oscillation (SO) is examined in the time domain by computing lagged cross correlations between sea level pressures at Darwin and sea level or surface pressures at selected stations. Also, in the Northern Hemisphere, the historical and US Navy sea level pressure analyses are used. All monthly time series are low-pass filtered to retain periodicities greater than 20 months in order to highlight the interannual fluctuations which are primarily associated with the SO. A detailed analysis of the post-1941 period results in plotted maps of the phase (lead or lag) and magnitude of the maximum cross correlations with Darwin, in a manner analogous to a broadband coherence and phase spectrum. The relationships within the SO are further examined, where possible, back to 1882 using time series of running decadal cross covariances. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 3078-3096 |
| Number of pages | 19 |
| Journal | Monthly Weather Review |
| Volume | 115 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1987 |
| Externally published | Yes |