Tropical cyclone activity (tropical depressions, tropical storms, and hurri
canes combined) in the central North Pacific has been found to be on the ri
se and this increase amounts to about 3.2 cyclones over the last 32 years (
1966-97). An examination of time series of tropical storms and hurricanes a
nd hurricane records alone also reveals an increasing trend in both series
since 1966.
The upward trend is characterized by decadal-scale variability as manifeste
d by fewer cyclones during the first half of the record (1966-81) and more
during the second half of the record (1982-97). The maximum hurricane inten
sity has also increased in the central North Pacific, as well as the number
of intense hurricanes from the first to the second half of the record. Rel
ative to 1966-81, sea surface temperatures in the tropical Pacific and rela
tive vorticity near the surface to the south of Hawaii have increased drama
tically during 1982-97. The changes in the frequency and intensity of tropi
cal cyclones in the central North Pacific appear to be modulated by decadal
-scale variability of the basic state of SST, which transitioned from a col
d to a warm phase in the late 1970s; this warm phase may have resulted in s
tronger and more frequent El Nino events as seen during the second half of
the record, leading to more cyclones in the central North Pacific.