On the difference in the net ecosystem exchange of CO2 between deciduous and evergreen forests in the southeastern United States

© 2014 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 21(2015), 2 vom: 28. Feb., Seite 827-42
1. Verfasser: Novick, Kimberly A (VerfasserIn)
Weitere Verfasser: Oishi, A Christopher, Ward, Eric J, Siqueira, Mario B S, Juang, Jehn-Yih, Stoy, Paul C
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2015
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. carbon flux drought eddy covariance evapotranspiration net ecosystem exchange water use efficiency wavelet spectra mehr... Carbon Dioxide 142M471B3J
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520 |a The southeastern United States is experiencing a rapid regional increase in the ratio of pine to deciduous forest ecosystems at the same time it is experiencing changes in climate. This study is focused on exploring how these shifts will affect the carbon sink capacity of southeastern US forests, which we show here are among the strongest carbon sinks in the continental United States. Using eight-year-long eddy covariance records collected above a hardwood deciduous forest (HW) and a pine plantation (PP) co-located in North Carolina, USA, we show that the net ecosystem exchange of CO2 (NEE) was more variable in PP, contributing to variability in the difference in NEE between the two sites (ΔNEE) at a range of timescales, including the interannual timescale. Because the variability in evapotranspiration (ET) was nearly identical across the two sites over a range of timescales, the factors that determined the variability in ΔNEE were dominated by those that tend to decouple NEE from ET. One such factor was water use efficiency, which changed dramatically in response to drought and also tended to increase monotonically in nondrought years (P < 0.001 in PP). Factors that vary over seasonal timescales were strong determinants of the NEE in the HW site; however, seasonality was less important in the PP site, where significant amounts of carbon were assimilated outside of the active season, representing an important advantage of evergreen trees in warm, temperate climates. Additional variability in the fluxes at long-time scales may be attributable to slowly evolving factors, including canopy structure and increases in dormant season air temperature. Taken together, study results suggest that the carbon sink in the southeastern United States may become more variable in the future, owing to a predicted increase in drought frequency and an increase in the fractional cover of southern pines 
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650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Research Support, U.S. Gov't, Non-P.H.S. 
650 4 |a carbon flux 
650 4 |a drought 
650 4 |a eddy covariance 
650 4 |a evapotranspiration 
650 4 |a net ecosystem exchange 
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700 1 |a Oishi, A Christopher  |e verfasserin  |4 aut 
700 1 |a Ward, Eric J  |e verfasserin  |4 aut 
700 1 |a Siqueira, Mario B S  |e verfasserin  |4 aut 
700 1 |a Juang, Jehn-Yih  |e verfasserin  |4 aut 
700 1 |a Stoy, Paul C  |e verfasserin  |4 aut 
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