Canadian Forest Service Publications

Interannual variability of net ecosystem productivity in forests is explained by carbon flux phenology in autumn. 2013. Wu, C.; Chen, J.M.; Black, T.A.; Price, D.T.; Kurz, W.A.; Desai, A.R.; Gonsamo, A.; Jassal, R.S.; Gough, C.M.; Bohrer, G.; Dragoni, D.; Herbst, M.; Gielen, B.; Berninger, F.; Vesala, T.; Mammarella, I.; Pilegaard, K.; Blanken, P.D. Global Ecology and Biogeography 22(8):994-1006.

Year: 2013

Available from: Pacific Forestry Centre

Catalog ID: 34367

Language: English

CFS Availability: PDF (request by e-mail)

Available from the Journal's Web site.
DOI: 10.1111/geb.12044

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Abstract

Aim To investigate the importance of autumn phenology in controlling interannual variability of forest net ecosystem productivity (NEP) and to derive new phenological metrics to explain the interannual variability of NEP.

Location North America and Europe.

Method Flux data from nine deciduous broadleaf forests (DBF) and 13 evergreen needleleaf forests (ENF) across North America and Europe (212 site-years) were used to explore the relationships between the yearly anomalies of annual NEP and several carbon flux based phenological indicators, including the onset/end of the growing season, onset/end of the carbon uptake period, the spring lag (time interval between the onset of growing season and carbon uptake period) and the autumn lag (time interval between the end of the carbon uptake period and the growing season). Meteorological variables, including global shortwave radiation, air temperature, soil temperature, soil water content and precipitation, were also used to explain the phenological variations.

Results We found that interannual variability of NEP can be largely explained by autumn phenology, i.e. the autumn lag. While variation in neither annual gross primary productivity (GPP) nor in annual ecosystem respiration (Re) alone could explain this variability, the negative relationship between annual NEP and autumn lag was due to a larger Re/GPP ratio in years with a prolonged autumn lag. For DBF sites, a longer autumn lag coincided with a significant decrease in annual GPP but showed no correlation with annual Re. However, annual GPP was insensitive to a longer autumn lag in ENF sites but annual Re increased significantly.

Main conclusions These results demonstrate that autumn phenology plays a more direct role than spring phenology in regulating interannual variability of annual NEP. In particular, the importance of respiration may be potentially underestimated in deriving phenological indicators.

Plain Language Summary

The goal of this paper was to understand how warmer autumns affect annual growth of forests and to investigate ways of capturing these effects in forest growth models. Data on forest growth and weather conditions measured at 22 boreal and temperate forests in Europe and North America were analysed to determine how year-to-year variations in climate affected different forests’ growth rates. Year-to-year variability in annual growth was found to be strongly related to autumn conditions: In conifer forests, longer autumns with warmer than normal weather were found to reduce net growth because respiration rates were higher while canopy photosynthesis was relatively unaffected. Conversely, in broadleaf forests, annual photosynthesis was reduced but respiration was not affected as much. The paper concludes that the timing of autumn cool-down is more important than the timing of spring warm-up in determining annual net growth rates of boreal and temperate forests. The importance of autumn respiration rates may have been underestimated in previous studies. This is important because with climate warming we can expect autumns to stay warmer longer, which will cause annual net forest growth to decline, with implications for the goods and services provided by forests.

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