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The Sub-Saharan Africa carbon balance, an overview
A. Bombelli1, M. Henry1,2,3, S. Castaldi4, S. Adu-Bredu5, A. Arneth6, A. de Grandcourt7,8, E. Grieco1, W. L. Kutsch9, V. Lehsten6, A. Rasile4, M. Reichstein9, K. Tansey10, U. Weber9, and R. Valentini1 1Department of Forest Environment and Resources (DISAFRI), University of Tuscia, via S. Camillo de Lellis, 01100 Viterbo, Italy 2Institut de Recherche pour le Développement, IRD, UR SeqBio, SupAgro, Bat. 12, 2 place Viala, 34060 Montpellier Cedex 1, France 3AgroParisTech-ENGREF, GEEFT, 648 rue Jean-François Breton, BP 7355, 34086 Montpellier Cedex 4, France 4Dipartimento di Scienze Ambientali, Seconda Università di Napoli, via Vivaldi 43, 81100 Caserta, Italy 5Forestry Research Institute of Ghana (FORIG), P.O. Box 63 KNUST, Kumasi, Ghana 6Department of Physical Geography and Ecosystems Analysis (INES), Centre for GeoBiosphere Science, Lund University, Sölvegatan 12, 223 62, Lund, Sweden 7Centre de coopération Internationale en Recherche Agronomique pour le Développement (CIRAD), Persyst, UPR80, TA B-80/D, 34398 Montpellier Cedex 5, France 8Unité de recherche sur la productivité des plantations industrielles (UR2PI), BP 1291, Pointe Noire, République du Congo 9Max-Planck Institute for Biogeochemistry, Hans-Knöll Strasse 10, 07745 Jena, Germany 10Department of Geography, University of Leicester, Leicester, LE1 7RH, UK
|  | Abstract. This study presents a summary overview of the carbon balance of Sub-Saharan
Africa (SSA) by synthesizing the available data from national communications
to UNFCCC and first results from the project CarboAfrica (net ecosystem
productivity and emissions from fires, deforestation and forest degradation,
by field and model estimates). According to these preliminary estimates the
overall carbon balance of SSA varies from 0.43 Pg C y−1 (using in situ
measurements for savanna NEP) to a much higher sink of 2.53 Pg C y−1
(using model estimates for savanna NEP). UNFCCC estimates lead to a moderate
carbon sink of 0.58 Pg C y−1. Excluding anthropogenic disturbance and
intrinsic episodic events, the carbon uptake by forests (0.98 Pg C y−1)
and savannas (from 1.38 to 3.48 Pg C y−1, depending on the used
methodology) are the main components of the SSA sink effect. Fires (0.72 Pg
C y−1), deforestation (0.25 Pg C y−1) and forest degradation (0.77 Pg
C y−1) are the main contributors to the SSA carbon emissions, while
the agricultural sector contributes only with 0.12 Pg C y−1. Notably,
the impact of forest degradation is higher than that caused by
deforestation, and the SSA forest net carbon balance is close to
equilibrium. Savannas play a major role in shaping the SSA carbon balance,
due to their large areal extent, their fire regime, and their strong
interannual NEP variability, but they are also a major uncertainty in the
overall budget. This paper shows that Africa plays a key role in the global
carbon cycle system and probably could have a potential for carbon
sequestration higher than expected, even if still highly uncertain. Further
investigations are needed, particularly to better address the role of
savannas and tropical forests. The current CarboAfrica network of carbon
measurements could provide future unique data sets for better estimating the
African carbon balance.
Discussion Paper (PDF, 1012 KB) Interactive Discussion (Closed, 4 Comments) Final Revised Paper (BG)
Citation: Bombelli, A., Henry, M., Castaldi, S., Adu-Bredu, S., Arneth, A., de Grandcourt, A., Grieco, E., Kutsch, W. L., Lehsten, V., Rasile, A., Reichstein, M., Tansey, K., Weber, U., and Valentini, R.: The Sub-Saharan Africa carbon balance, an overview, Biogeosciences Discuss., 6, 2085-2123, 2009. Bibtex EndNote Reference Manager
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