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Impacts of climate change on savannah woodland biomass carbon density and water-use: a modelling study of the Sudanese gum belt region

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Abstract

This paper analyzes potential impacts of climate change on biomass carbon (C) density and water-use (actual evapotranspiration, AET) of savannah woodlands in Sudan. Climate change scenarios were developed from five General Circulation Models (GCMs; CGCM2, CSIRO2, ECHam4, HadCM3 and PCM) under two IPCC (Intergovernmental Panel on Climate Change) emission scenarios (A1FI and B1). Baseline (1961-90) climate and climate change scenarios for 2080s for eight map sheet grids (1° latitude x 1.5° longitude) were constructed. Compared to baseline values, mean annual precipitation (MAP) showed both increases (+112 to +221 mm) and decreases (−13 to −188 mm) but mean annual temperature (MAT) only showed increases (+1.2 to +8.3 °C). Baseline biomass C densities showed an exponential relationship with MAP (y = 6.798 e 0.0054x, R2 = 0.70). Depending on climate change MAP, biomass C densities increased (+14 to +241 g C m−2) or decreased (−1 to −148 g C m−2). However, because of uncertainty in biomass C density estimates, the changes were only significant (P <0.05) for some of the climate change scenarios and for grids with MAP >260 mm. Under A1FI emission scenarios, only HadCM3 did not have a significant effect while under B1 emission scenarios, only CGCM2 and ECHam4 had a significant effect on biomass C density. AET also showed both increases (+100 to +145 mm for vertisols and +82 to +197 mm for arenosols) and decreases (−12 to −178 mm for vertisols and −12 to −132 mm for arenosols). The largest relative changes in AET (up to 31 %) were associated with grids receiving the lowest rainfall. Thus, even if MAP increases across the study region, the increase will have little impact on biomass levels in the driest areas of the region, emphasizing the need for improved management and use of savannah woodlands.

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Acknowledgments

This study is mainly financed by the Graduate School in Forest Sciences (GSForest), Finland. The authors would like to thank Professor Tim Carter and Mr. Stefan Fronzek (Finnish Environment institute, Finland) for their fruitful discussion on the use of GCMs and SRES emission scenarios for constructing climate change scenarios. The authors also wish to thank Dr Paul J. Krusic (Department of Physical Geography and Quaternary Geology, Stockholm University) for providing the idea of using TETYN software for unpacking the climate parameters from CRU TS 2.1 and TYN SC 2.03 dataset. Dr Norbert Solymosi (Adaptation to Climate Change Research Group, Hungarian Academy of Sciences, Budapest, Hungary) is thanked for his support to remove the bug in TETYN software to work with ECHam4 GCM model run with B1 emission scenario based on our recommendation.

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Alam, S.A., Starr, M. Impacts of climate change on savannah woodland biomass carbon density and water-use: a modelling study of the Sudanese gum belt region. Mitig Adapt Strateg Glob Change 18, 979–999 (2013). https://doi.org/10.1007/s11027-012-9403-5

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