Results/Conclusions: Results indicate that 53% of long-term mean NPP can be accounted for by climatic conditions; important climate variables (all positive relationships) included spring precipitation (r2=0.17), annual temperature (r2=0.48) and temperature in winter, spring, summer and fall (r2=0.32, 0.46, 0.37 and 0.44, respectively.) NPP variability was only weakly related to climate. Forest types displayed differences in NPP mean and variability, but those differences were not statistically significant after controlling for climate. 54% of annual NPP deviations could be accounted for by weather fluctuations; important weather precipitation included annual, winter and fall precipitation in the prior year and winter precipitation two years prior while important weather temperature (all positive) included annual, spring and fall temperatures in the current year, and spring temperature two years prior. Relationships between NPP deviations and weather fluctuations differed among forest types in magnitude, although not in direction. These differences in NPP-weather relationships among forest types remained statistically significant even after controlling for climate, suggesting subtle evidence for forest type complimentarity. In addition, even after controlling for climate, forest type evenness was positively related to long-term mean NPP and negatively related to NPP variability, suggesting that greater functional diversity may enhance NPP sustainability.