Extreme phases of the El Nino-Southern Oscillation (ENSO) phenomenon have b
een blamed for precipitation anomalies in many areas of the world. In some
areas the probability of above-normal precipitation may be increased during
warm or cold events. while in others below-normal precipitation may be mor
e likely. The percentages of times that seasonal precipitation over land ar
eas was above, near, and below normal during the eight strongest El Nino an
d La Nina episodes are tabulated, and the significance levels of the poster
ior probabilities are calculated using the hypergeometric distribution. The
se frequencies may provide a useful starting point for probabilistic climat
e forecasts during strong ENSO events. Areas with significantly high or low
frequencies or above- or below-normal precipitation are highlighted, and a
ttempts are made to estimate the proportion of land areas with significant
ENSO-related precipitation signals.
There is a danger of overstating the global impact of ENSO events because o
nly about 20%-30% of land areas experience significantly increased probabil
ities of above- or below-normal seasonal precipitation during at least some
part of the year. Since different areas are affected at different times of
the year, the fraction of global land affected in any particular season is
only about 15%-25%. The danger of focusing on the impact of only warm-phas
e events is emphasized also: the global impact of La Nina seems to be at le
ast as widespread as that of El Nino. Furthermore, there are a number of no
table asymmetries in precipitation responses to El Nino and La Nina events.
For many areas it should not be assumed that the typical climate anomaly o
f one ENSO extreme is likely to be the opposite of the other extreme. A hig
h frequency of above-normal precipitation during strong El Nine conditions,
for example. does not guarantee a high frequency of below-normal precipita
tion during La Nina events, or vice versa. On a global basis El Nino events
are predominantly associated with below-normal seasonal precipitation over
land, whereas La Nina events result in a wider extent of above-normal prec
ipitation.