Modelling biome shifts and tree cover change for 2050 in West Africa

被引:45
作者
Heubes, Jonathan [1 ]
Kuehn, Ingolf [2 ]
Koenig, Konstantin [1 ,3 ]
Wittig, Ruediger [1 ,4 ]
Zizka, Georg [1 ,4 ,5 ,6 ]
Hahn, Karen [1 ,4 ]
机构
[1] Biodivers & Climate Res Ctr LOEWE BiK F, D-60325 Frankfurt, Germany
[2] UFZ Helmholtz Ctr Environm Res, Helmholtz Ctr Environm Res UFZ, D-06120 Halle, Germany
[3] EMBRAPA Amazonia Oriental, World Agroforestry Ctr ICRAF, Amazon Initiat Consortium, BR-66095100 Belem, Para, Brazil
[4] Goethe Univ Frankfurt, Inst Ecol Evolut & Divers, D-60323 Frankfurt, Germany
[5] Senckenberg Res Inst, D-60325 Frankfurt, Germany
[6] Nat Hist Museum, D-60325 Frankfurt, Germany
关键词
Africa; bioclimatic envelope models; climate change; desertification; forest degradation; generalized additive model; human impact; species distribution modelling; CLIMATE-CHANGE; SPECIES DISTRIBUTIONS; LAND-COVER; SAHARA DESERT; VEGETATION; BIODIVERSITY; IMPACTS; DESERTIFICATION; PATTERNS; SAHEL;
D O I
10.1111/j.1365-2699.2011.02560.x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Aim Africa is expected to face severe changes in climatic conditions. Our objectives are: (1) to model trends and the extent of future biome shifts that may occur by 2050, (2) to model a trend in tree cover change, while accounting for human impact, and (3) to evaluate uncertainty in future climate projections. Location West Africa. Methods We modelled the potential future spatial distribution of desert, grassland, savanna, deciduous and evergreen forest in West Africa using six bioclimatic models. Future tree cover change was analysed with generalized additive models (GAMs). We used climate data from 17 general circulation models (GCMs) and included human population density and fire intensity to model tree cover. Consensus projections were derived via weighted averages to: (1) reduce inter-model variability, and (2) describe trends extracted from different GCM projections. Results The strongest predicted effect of climate change was on desert and grasslands, where the bioclimatic envelope of grassland is projected to expand into the desert by an area of 2 million km(2). While savannas are predicted to contract in the south (by 54 +/- 22 x 10(4) km(2)), deciduous and evergreen forest biomes are expected to expand (64 +/- 13 x 10(4) km(2) and 77 +/- 26 x 10(4) km(2)). However, uncertainty due to different GCMs was particularly high for the grassland and the evergreen biome shift. Increasing tree cover (1-10%) was projected for large parts of Benin, Burkina Faso, Cote d'Ivoire, Ghana and Togo, but a decrease was projected for coastal areas (1-20%). Furthermore, human impact negatively affected tree cover and partly changed the direction of the projected change from increase to decrease. Main conclusions Considering climate change alone, the model results of potential vegetation (biomes) show a 'greening' trend by 2050. However, the modelled effects of human impact suggest future forest degradation. Thus, it is essential to consider both climate change and human impact in order to generate realistic future tree cover projections.
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页码:2248 / 2258
页数:11
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