Various indications for shifts in plant and animal phenology resulting from
climate change have been observed in Europe. This analysis of phenological
seasons in Germany of more than four decades (1951-96) has several major a
dvantages: (i) a wide and dense geographical coverage of data from the phen
ological network of the German Weather Service, (ii) the 16 phenophases ana
lysed cover the whole annual cycle and, moreover, give a direct estimate of
the length of the growing season for four deciduous tree species. After in
tensive data quality checks, two different methods -linear trend analyses a
nd comparison of averages of subintervals - were applied in order to determ
ine shifts in phenological seasons in the last 46 years. Results from both
methods were similar and reveal a strong seasonal variation. There are clea
r advances in the key indicators of earliest and early spring (-0.18 to -0.
23 d y(-1)) and notable advances in the succeeding spring phenophases such
as leaf unfolding of deciduous trees (-0.16 to -0.08 d y(-1)). However, phe
nological changes are less strong during autumn (delayed by +0.03 to + 0.10
d y(-1) on average). In general, the growing season has been lengthened by
up to -0.2 d y(-1) (mean linear trends) and the mean 1974-96 growing seaso
n was up to 5 days longer than in the 1951-73 period. The spatial variabili
ty of trends was analysed by statistical means and shown in maps, but these
did not reveal any substantial regional differences. Although there is a h
igh spatial variability, trends of phenological phases at single locations
are mirrored by subsequent phases, but they are not necessarily identical.
Results for changes in the biosphere with such a high resolution with respe
ct to time and space can rarely be obtained by other methods such as analys
es of satellite data.