A phenological study of springtime events was made over a 61-year period at
one site in southern Wisconsin. The records over this long period show tha
t several phenological events have been increasing in earliness; we discuss
evidence indicating that these changes reflect climate change. The mean of
regressions for the 55 phenophases studied was -0.12 day per year, an over
all increase in phenological earliness at this site during the period. Some
phenophases have not increased in earliness, as would be expected for phen
ophases that are regulated by photoperiod or by a physiological signal othe
r than local temperature.