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Deforestation and India


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             As indicated, one of the major causes of the deforestation in the Indonesian Sumatra rainforest is the logging for timber trade (Weatherbee 47). About 36 hectares of forest cover are cleared daily as a result of timber harvesting. Apart from the unsustainable logging, other factors such as fuel wood harvesting, climate change and conversion of forest cover for farming and infrastructure development have also accounted for the clearance of natural forest in Indonesia (Brown and Pearce 13). As mentioned, the results range from reduced biodiversity to disruption of livelihoods. The other effects include increased greenhouse gas emissions, disrupted water cycle and increased soil erosions. .
             Climate change due to deforestation is largely due to greenhouse gases in the tropical region (Franchito 76). Studies indicate that tropical forests such as that found in Indonesia hold over 200 gigatonnes of carbon (White 53). Destruction of such forests release large volumes of carbon into the atmosphere. Essentially, it is estimated that the destruction of Indonesian natural forests accounts for over 50% of the total forest carbon release into the atmosphere (White 54). On a global level, warming due to deforestation accounts for around 60% of the warming in the tropical region when carbon increase is factored in. The increase of carbon concentration increases the change in the surface temperature due to the deforestation by 60% "75% in the tropical land region (Franchito 75).
             In addition to carbon increase, deforestation correlates with decreased evapotranspiration, precipitation and net surface radiation in the tropical region (Franchito 74). The reduction in evapotranspiration and net longwave radiation flux that leaves the Earth is responsible for the increase of surface temperature, which leads to a warmer and drier climate (Franchito 74). Carbon concentration increase results in reduction of evapotranspiration and precipitation by 7 "12% and net surface radiation reducation by 48% "58% in the tropical regions (Franchito 79).


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