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Data-driven diagnostics of terrestrial carbon dynamics over North America

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Title Data-driven diagnostics of terrestrial carbon dynamics over North America
Names Xiao, Jingfeng (creator)
Ollinger, Scott V. (creator)
Frolking, Steve (creator)
Law, Bevery E. (creator)
et al. (creator)
Date Issued 2014-10-15 (iso8601)
Note To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/agricultural-and-forest-meteorology.
Abstract The exchange of carbon dioxide is a key measure of ecosystem metabolism and a critical intersection
between the terrestrial biosphere and the Earth’s climate. Despite the general agreement that
the terrestrial ecosystems in North America provide a sizeable carbon sink, the size and distribution
of the sink remain uncertain. We use a data-driven approach to upscale eddy covariance flux observations
from towers to the continental scale by integrating flux observations, meteorology, stand age,
aboveground biomass, and a proxy for canopy nitrogen concentrations from AmeriFlux and Fluxnet-Canada Research Network as well as a variety of satellite data streams from the MODIS sensors. We
then use the resulting gridded flux estimates from March 2000 to December 2012 to assess the magnitude,
distribution, and interannual variability of carbon fluxes for the U.S. and Canada. The mean
annual gross primary productivity (GPP), ecosystem respiration (ER), and net ecosystem productivity
(NEP) of the U.S. over the period 2001–2012 were 6.84, 5.31, and 1.10 Pg C yr⁻¹, respectively; the mean
annual GPP, ER, and NEP of Canada over the same 12-year period were 3.91, 3.26, and 0.60 Pg C yr⁻¹,
respectively. The mean nationwide annual NEP of natural ecosystems over the period 2001–2012 was
0.53 Pg C yr⁻¹ for the U.S. and 0.49 Pg C yr⁻¹ for the conterminous U.S. Our estimate of the carbon
sink for the conterminous U.S. was almost identical with the estimate of the First State of the Carbon
Cycle Report (SOCCR). The carbon fluxes exhibited relatively large interannual variability over the
study period. The main sources of the interannual variability in carbon fluxes included drought and
disturbance. The annual GPP and NEP were strongly related to annual evapotranspiration (ET) for both the U.S. and Canada, showing that the carbon and water cycles were closely coupled. Our gridded flux
estimates provided an independent, alternative perspective on ecosystem carbon exchange over North
America.
Genre Article
Topic Carbon sink
Identifier Xiao, J., Ollinger, S. V., Frolking, S., Hurtt, G. C., Hollinger, D. Y., Davis, K. J., ... & Suyker, A. E. (2014). Data-driven diagnostics of terrestrial carbon dynamics over North America. Agricultural and Forest Meteorology, 197, 142-157. doi:10.1016/j.agrformet.2014.06.013

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