Net carbon uptake has increased through warming-induced changes in temperate forest phenology

Trevor F. Keenan (), Josh Gray, Mark A. Friedl, Michael Toomey, Gil Bohrer, David Y. Hollinger, J. William Munger, John O’Keefe, Hans Peter Schmid, Ian Sue Wing, Bai Yang and Andrew D. Richardson
Additional contact information
Trevor F. Keenan: Macquarie University
Josh Gray: Boston University
Mark A. Friedl: Boston University
Michael Toomey: Harvard University
Gil Bohrer: Environmental & Geodetic Eng., The Ohio State University
David Y. Hollinger: USDA Forest Service, Northern Research Station
J. William Munger: Harvard University
John O’Keefe: Harvard Forest
Hans Peter Schmid: Inst. of Meteorology and Climate Research, Karlsruhe Institute of Technology
Ian Sue Wing: Boston University
Bai Yang: Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory
Andrew D. Richardson: Harvard University

Nature Climate Change, 2014, vol. 4, issue 7, 598-604

Abstract: The timing of life-history events has a strong impact on ecosystems. Now, analysis of the phenology of temperate forests in the eastern US indicates that in the case of an earlier spring and a later autumn, carbon uptake (photosynthesis) increases considerably more than carbon release (respiration).

Date: 2014
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DOI: 10.1038/nclimate2253

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