There has been an apparent increase in the frequency and duration of E
l Nino-Southern Oscillation events in the last two decades relative to
the prior period of record. Furthermore, 1990-95 was the longest peri
od of sustained high Darwin sea level pressure in the instrumental rec
ord. Variations in the frequency and duration of such events are of co
nsiderable interest because of their implications for understanding gl
obal climatic variability and also the possibility that the climate sy
stem may be changing due to external factors such as the increased con
centration of greenhouse gases in the atmosphere. Nonparametric statis
tical methods for time series analysis are applied to a 1882 to 1995 s
easonal Darwin sea level pressure (DSLP) anomaly time series to explor
e the variations in El Nino-like anomaly occurrence and persistence ov
er the period of record. Return periods for the duration of the 1990-9
5 event are estimated to be considerably smaller than those recently o
btained by Trenberth and Hear using a linear ARMA model with the same
time series. The likelihood of a positive anomaly of the DSLP, as well
as its persistence, is found to exhibit decadal- to centennial-scale
variability and was nearly as high at the end of the last century as i
t has been recently. The 1990-95 event has a much lower return period
if the analysis is based on the 1882-1921 DSLP data. The authors sugge
st that conclusions that the 1990-95 event may be an effect of greenho
use gas-induced warming be tempered by a recognition of the natural va
riability in the system.