Ma. White et al., A CONTINENTAL PHENOLOGY MODEL FOR MONITORING VEGETATION RESPONSES TO INTERANNUAL CLIMATIC VARIABILITY, Global biogeochemical cycles, 11(2), 1997, pp. 217-234
Regional phenology is important in ecosystem simulation models and cou
pled biosphere/atmosphere models. In the continental United States, th
e timing of the onset of greenness in the spring (leaf expansion, gras
s green-up) and offset of greenness in the fall (leaf abscission, cess
ation of height growth, grass brown-off) are strongly influenced by me
teorological and climatological conditions. We developed predictive ph
enology models based on traditional phenology research using commonly
available meteorological and climatological data. Predictions were com
pared with satellite phenology observations at numerous 20 km x 20 km
contiguous landcover sites. Onset mean absolute error was 7.2 days in
the deciduous broadleaf forest (DBF) biome and 6.1 days in the grassla
nd biome. Offset mean absolute error was 5.3 days in the DBF biome and
6.3 days in the grassland biome. Maximum expected errors at a 95% pro
bability level ranged from 10 to 14 days. Onset was strongly associate
d with temperature summations in both grassland and DBF biomes; DBF of
fset was best predicted with a photoperiod function, while grassland o
ffset required a combination of precipitation and temperature controls
. A long-term regional test of the DBF onset model captured field-meas
ured interannual variability trends in lilac phenology. Continental ap
plication of the phenology models for 1990-1992 revealed extensive int
erannual variability in onset and offset. Median continental growing s
eason length ranged from a low of 129 days in 1991 to a high of 146 da
ys in 1992. Potential uses of the models include regulation of the tim
ing and length of the growing season in large-scale biogeochemical mod
els and monitoring vegetation response to interannual climatic variabi
lity.