Premise of the Study
We investigated the spatial and temporal patterns of vegetation phenology with phenometrics derived from PhenoCam imagery. Specifically, we evaluated the Bioclimatic Law proposed by Hopkins, which relates phenological transitions to latitude, longitude, and elevation.
Methods
“Green‐up” and “green‐down” dates—representing the start and end of the annual cycles of vegetation activity—were estimated from measures of canopy greenness calculated from digital repeat photography. We used data from 65 deciduous broadleaf (
DB
) forest sites, 18 evergreen needleleaf (
EN
) forest sites, and 21 grassland (
GR
) sites.
Results
DB
green‐up dates were well correlated with mean annual temperature and varied along spatial gradients consistent with the Bioclimatic Law. Interannual variation in
DB
phenology was most strongly associated with temperature anomalies during a relatively narrow window of time.
EN
phenology was not well correlated with either climatic factors or spatial gradients, but similar to
DB
phenology, interannual variation was most closely associated with temperature anomalies. For
GR
sites, mean annual precipitation explained most of the spatial variation in the duration of vegetation activity, whereas both temperature and precipitation anomalies explained interannual variation in phenology.
Discussion
PhenoCam data provide an objective and consistent means by which spatial and temporal patterns in vegetation phenology can be investigated.