Europe's Terrestrial Biosphere Absorbs 7 to 12% of European Anthropogenic CO 2 Emissions

Author:

Janssens Ivan A.12345,Freibauer Annette12345,Ciais Philippe12345,Smith Pete12345,Nabuurs Gert-Jan12345,Folberth Gerd12345,Schlamadinger Bernhard12345,Hutjes Ronald W. A.12345,Ceulemans Reinhart12345,Schulze E.-Detlef12345,Valentini Riccardo12345,Dolman A. Johannes12345

Affiliation:

1. Department of Biology, Universiteit Antwerpen, B-2160 Antwerpen, Belgium.

2. Max Planck Institute for Biogeochemistry, 07701 Jena, Germany.

3. Laboratoire des Sciences du Climat et de l'Environnement, 91191 Gif sur Yvette, France.

4. Department of Plant and Soil Science, University of Aberdeen, Aberdeen AB24 3FX, UK.

5. Alterra Green World Research, Wageningen, 6700 AC, Netherlands.

Abstract

Most inverse atmospheric models report considerable uptake of carbon dioxide in Europe's terrestrial biosphere. In contrast, carbon stocks in terrestrial ecosystems increase at a much smaller rate, with carbon gains in forests and grassland soils almost being offset by carbon losses from cropland and peat soils. Accounting for non–carbon dioxide carbon transfers that are not detected by the atmospheric models and for carbon dioxide fluxes bypassing the ecosystem carbon stocks considerably reduces the gap between the small carbon-stock changes and the larger carbon dioxide uptake estimated by atmospheric models. The remaining difference could be because of missing components in the stock-change approach, as well as the large uncertainty in both methods. With the use of the corrected atmosphere- and land-based estimates as a dual constraint, we estimate a net carbon sink between 135 and 205 teragrams per year in Europe's terrestrial biosphere, the equivalent of 7 to 12% of the 1995 anthropogenic carbon emissions.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference50 articles.

1. A Large Northern Hemisphere Terrestrial CO 2 Sink Indicated by the 13 C/ 12 C Ratio of Atmospheric CO 2

2. Climate Change 2001: The Scientific Basis 2001

3. Towards robust regional estimates of CO2 sources and sinks using atmospheric transport models

4. The net exchange of C between an ecosystem such as a forest and the atmosphere is NEP. Although NEP is a good measure for C sequestration at annual time scales it is not an appropriate indicator of C sequestration at the continental scale and over longer time periods ( 48 ). European forests are predominantly production forests and a large fraction of NEP is removed from forests at thinning and harvest. In addition disturbances such as pest outbreaks and forest fires can remove large quantities of C from forests. What remains in the forest after harvest and disturbances is NBP ( 48 ) and it is NBP rather than NEP that determines the long-term sink and the atmosphericsignal of the C balance of European forests.

5. Biomass and Carbon Budget of European Forests, 1971 to 1990

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