Citation Information

  • Title : Reconciling estimates of the contemporary North American carbon balance among terrestrial biosphere models, atmospheric inversions, and a new approach for estimating net ecosystem exchange from inventory-based data.
  • Source : Global Change Biology
  • Publisher : Wiley-Blackwell
  • Volume : 18
  • Issue : 4
  • Pages : 1282-1299
  • Year : 2012
  • DOI : 10.1111/j.1365-2486.2011.02627.x
  • ISBN : 1354-1013
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Kurz, W. A.
    • Birdsey, R. A.
    • McConkey, B. G.
    • Dejong, B.
    • Heath, L. S.
    • West, T. O.
    • Wei, Y. X.
    • McGuire, A. D.
    • Stinson, G.
    • Turner, D. P.
    • Hayes, D. J.
    • Jacobson, A. R.
    • Huntzinger, D. N.
    • Pan, Y. D.
    • Post, W. M.
    • Cook, R. B.
  • Climates:
  • Cropping Systems:
  • Countries: USA. Mexico. Canada.

Summary

We develop an approach for estimating net ecosystem exchange (NEE) using inventory-based information over North America (NA) for a recent 7-year period (ca. 2000-2006). The approach notably retains information on the spatial distribution of NEE, or the vertical exchange between land and atmosphere of all non-fossil fuel sources and sinks of CO 2, while accounting for lateral transfers of forest and crop products as well as their eventual emissions. The total NEE estimate of a -327252 TgC yr -1 sink for NA was driven primarily by CO 2 uptake in the Forest Lands sector (-248 TgC yr -1), largely in the Northwest and Southeast regions of the US, and in the Crop Lands sector (-297 TgC yr -1), predominantly in the Midwest US states. These sinks are counteracted by the carbon source estimated for the Other Lands sector (+218 TgC yr -1), where much of the forest and crop products are assumed to be returned to the atmosphere (through livestock and human consumption). The ecosystems of Mexico are estimated to be a small net source (+18 TgC yr -1) due to land use change between 1993 and 2002. We compare these inventory-based estimates with results from a suite of terrestrial biosphere and atmospheric inversion models, where the mean continental-scale NEE estimate for each ensemble is -511 TgC yr -1 and -931 TgC yr -1, respectively. In the modeling approaches, all sectors, including Other Lands, were generally estimated to be a carbon sink, driven in part by assumed CO 2 fertilization and/or lack of consideration of carbon sources from disturbances and product emissions. Additional fluxes not measured by the inventories, although highly uncertain, could add an additional -239 TgC yr -1 to the inventory-based NA sink estimate, thus suggesting some convergence with the modeling approaches.

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