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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Alpine grasslands response to climatic factors and anthropogenic activities on the Tibetan Plateau from 2000 to 2012
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Alpine grasslands response to climatic factors and anthropogenic activities on the Tibetan Plateau from 2000 to 2012

机译:2000年至2012年青藏高原高寒草原对气候因子和人为活动的响应

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To address pasture degradation on the Tibetan Plateau, the Chinese government has launched the ecological restoration project Grazing Withdrawal Program (GWP) since 2004. However, few studies have evaluated the impact of the GWP on grassland recovery. Based on monthly remote-sensed vegetation index and meteorological data from 2000 to 2012, we assessed the dynamics of annual net primary productivity (NPP) in alpine grasslands and quantified the effects of climatic factors and anthropogenic activities on NPP change by using the climate-driven NPP and the Carnegie-Ames-Stanford Approach (CASA) models. We found that there existed two distinct periods with an accelerating trend in NPP increase before and after 2004. The area percentage of NPP change induced by climatic factors increased from 41.55% to 83.75%, but that percentage caused by human activities decreased from 58.45% to 16.25% in the two periods of 2000-2004 and 2004-2012. Between 2000 and 2004, overgrazing reduced the positive effect of climate change on NPP variability, resulting in wide-scale grassland degradation. Between 2004 and 2012, grassland ecosystems gradually recovered from heavy grazing pressure, and the human induced degradation was reversed after the implementation of the GWP. Thus, temperature and solar radiation became dominant factors in driving NPP change. Our results indicated that the GWP produces a significant positive effect on the restoration of alpine grasslands by controlling livestock numbers and decreasing grazing intensity. This study provides an objective assessment of restoration actuation on grassland ecosystems, having important implications for demonstrating the effectiveness of the GWP on grassland restoration on the Tibetan Plateau. (C) 2016 Elsevier B.V. All rights reserved.
机译:为了解决青藏高原的牧草退化问题,中国政府自2004年起启动了生态恢复项目放牧退耕计划(GWP)。但是,很少有研究评估GWP对草地恢复的影响。基于2000年至2012年的月度遥感植被指数和气象数据,我们评估了高寒草地年净初级生产力(NPP)的动态,并通过气候驱动量化了气候因素和人为活动对NPP变化的影响NPP和卡内基-埃姆斯-斯坦福方法(CASA)模型。我们发现有两个明显的时期,2004年之前和之后的NPP都有加速增长的趋势。气候因素引起的NPP变化的面积百分比从41.55%增加到83.75%,但是人类活动引起的NPP变化的百分比从58.45%下降到在2000-2004年和2004-2012年的两个时期中,分别为16.25%。在2000年至2004年之间,过度放牧降低了气候变化对NPP变异性的积极影响,导致了草原的大规模退化。在2004年至2012年期间,草原生态系统从沉重的放牧压力中逐渐恢复,在实施全球升温潜能值后,人为引起的退化得以逆转。因此,温度和太阳辐射成为驱动NPP变化的主要因素。我们的结果表明,GWP通过控制牲畜数量和降低放牧强度,对高寒草原的恢复产生了显着的积极影响。这项研究提供了对草地生态系统恢复驱动的客观评估,对证明全球升温潜能值对青藏高原草地恢复的有效性具有重要意义。 (C)2016 Elsevier B.V.保留所有权利。

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