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Impacts of climate and land-cover changes in arid lands of Central Asia

机译:气候和中亚干旱地区土地覆盖变化的影响

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摘要

Despite the growing understanding of the global climate change, great uncertainties exist in the prediction of responses of arid regions to global and regional, natural and human-induced climate change. Meteorological data series show a steady increase of annual and winter temperatures in Central Asia since the beginning of the 20th century that might have a strong potential impact on the region's natural ecosystems, agricultural crops, and human health. Analyses of the NOAA AVHRR temporal series since the 1980s showed a decrease in aridity from 1991-2000 compared to 1982-1990. While most climate models agree that the temperature in arid Central Asia will increase by 1-2℃ by 2030-2050, precipitation projections vary from one model to another and projected changes in the aridity index for different model runs show no consistent trend for this region. Local and regional human impacts in arid zones can significantly modify surface albedo, as well as water exchange and nutrient cycles that could have impacts on the climatic system both at the regional and global scales.
机译:尽管人们对全球气候变化的认识越来越高,但在预测干旱地区对全球和区域,自然和人为引起的气候变化的反应方面存在很大的不确定性。气象数据系列显示,自20世纪初以来,中亚的年度和冬季温度稳定上升,这可能对该地区的自然生态系统,农作物和人类健康产生巨大的潜在影响。自1980年代以来对NOAA AVHRR时间序列的分析表明,与1982-1990年相比,1991-2000年的干旱减少了。尽管大多数气候模型都认为到2030-2050年干旱中亚的温度将升高1-2℃,但降水预测因一种模型而异,并且不同模型运行的干旱指数预测变化在该地区没有一致的趋势。 。干旱地区的局部和区域人类影响可以显着改变地表反照率,以及可能对区域和全球范围的气候系统产生影响的水交换和养分循环。

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