2018
DOI: 10.3390/cli6020035
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Simulating the Impacts of Tree, C3, and C4 Plant Functional Types on the Future Climate of West Africa

Abstract: This study investigates the future climatic impacts of different percentages of trees/shrubs, C4 and C3 plant functional types (PFTs) over the West Africa region. The ratio of co-existence among the different PFTs was done as a representation of agri-silviculture practices over the region. Nine sensitivity experiments of different percentages of trees/shrubs, and C4 and C3 PFTs were carried out with a regional climate model (RegCM4) driven by Global Climate Model (HADGEM2-ES) outputs. These experiments were ca… Show more

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Cited by 4 publications
(3 citation statements)
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“…New forests could also affect temperatures by providing local cooling. 186,188 These results highlight the importance of land-use policies in future projections of climate extremes, especially in a region that is already experiencing a significant increase in extreme precipitation events 189 and it likely to experience violent heat waves in the future. 190 A looming issue for future afforestation plans is the potential climatic impacts on remote regions, which so far have been investigated in detail by only a handful of studies.…”
Section: Recent and Projected Vegetation Changesmentioning
confidence: 84%
“…New forests could also affect temperatures by providing local cooling. 186,188 These results highlight the importance of land-use policies in future projections of climate extremes, especially in a region that is already experiencing a significant increase in extreme precipitation events 189 and it likely to experience violent heat waves in the future. 190 A looming issue for future afforestation plans is the potential climatic impacts on remote regions, which so far have been investigated in detail by only a handful of studies.…”
Section: Recent and Projected Vegetation Changesmentioning
confidence: 84%
“…Here are three examples where this is the case: (i) C 4 grasslands in the highveld of southern Africa, dominated by Hyparrhenia hirta (L.) Stapf (Panicoideae) and Sporobolus pyramidalis P.Beauv. (Chloridoideae) receive an annual mean precipitation between 400 and 900 mm mainly during the warm summer months (Bond, 2008 ; Low & Rebelo, 1996 ; Mills & Cowling, 2006 ); (ii) species‐rich C 4 grasslands at the tropical Sudanian savanna near the Volta‐, Benue‐ and Niger‐River experience a peak of summer precipitation of 600 mm in the north and 1000 mm in the south and the West African monsoons that occur between June and August result in warmer and wetter summers that support C 4 vegetation (Olusegun et al., 2018 ); (iii) species‐rich C 4 grasslands in north‐east Queensland and the Northern Territory, Australia, are associated with the tropical to subtropical climate along the coastal strip, the warm and wet summer months (December–February) and the Australian monsoon bringing up to 1300 mm rainfall (Ondei et al., 2016 ).…”
Section: Discussionmentioning
confidence: 99%
“…Indeed, Kamoni and Gicheru (2015) pinpoint that "Sustainable land management practices enhance carbon sequestration and sustain agricultural productivity, thus mitigating against climate change" (p. 307). Agroforestry Mutuo et al, 2005;Olusegun et al, 2018) is also considered as a means to increase carbon sequestration and reduce GHG emissions. Mutuo et al (2005) suggest that "Evidence is emerging that agroforestry systems are promising management practices to increase aboveground and soil C stocks and reduce soil degradation, as well as to mitigate greenhouse gas emissions" (p. 43).…”
Section: Climate Change Mitigation and Adaptationmentioning
confidence: 99%