Timely detection of changes in the tropical Pacific and subsequent predicti
ons that the west coast of North America would be impacted by a strong El N
ino event in 1997 enabled CalCOFI to augment its time-series sampling to pr
ovide monthly coverage of a subset of the sample grid. The 1997-98 El Nino
event in California waters is described here ill terms of a preliminary tim
eline of events. This improved description of the timing of changes in the
CalCOFI region provides new insights into the types of changes that might b
e expected during future events, and it also constitutes a natural experime
nt which can be used to test hypotheses about the cause-and-effect mechanis
ms linking changing physical structure with ecosystem impacts. Although som
e effects attributed to El Nino were evident in the summer and fall of 1997
, the strongest occurred in winter 1997-98 and spring 1998. Advection and c
hanges in ranges of mobile populations were consistent with the northward e
xtension of the range of southern warm-water species of migratory game fish
and plankton. However, the timeline observations were not consistent with
predictions based upon a simple model of bottom-up trophic processes (chang
es in physical structure, nutrients, phytoplankton, zooplankton, upper trop
hic levels) as the mechanism linking changing physical and ecosystem struct
ure. While not surprising, since few simple models have much skill in predi
cting structure in natural ecosystems, this suggests that ecosystems manage
rs will have to await a better understanding of cause-and-effect linkages b
efore improved skill in observing and predicting the physical effects of El
Nino upon California waters can be directly translated into improved skill
in predicting ecosystem effects.