How global warming affect the desertification process is not 100% understood, but it is clear that an elevation in atmospheric and ground-level temperatures is likely to aggravate soil and vegetation loss in already hot climes. An increase in evapotranspiration and the decrease in rainfall mean that already semi-arid and sub-humid areas found across the world would face a future barrenness that is almost irreversible. This would negatively affect biodiversity and have a major impact on local human cultures and wildlife.
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