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首页> 外文期刊>Ecology and Evolution >Effects of climate warming on net primary productivity in China during 1961?¢????2010
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Effects of climate warming on net primary productivity in China during 1961?¢????2010

机译:气候变暖对1961年中国净初级生产力的影响?¢???? 2010

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Abstract The response of ecosystems to different magnitudes of climate warming and corresponding precipitation changes during the last few decades may provide an important reference for predicting the magnitude and trajectory of net primary productivity (NPP) in the future. In this study, a process-based ecosystem model, Carbon Exchange between Vegetation, Soil and Atmosphere (CEVSA), was used to investigate the response of NPP to warming at both national and subregional scales during 1961?¢????2010. The results suggest that a 1.3???°C increase in temperature stimulated the positive changing trend in NPP at national scale during the past 50 years. Regardless of the magnitude of temperature increase, warming enhanced the increase in NPP; however, the positive trend of NPP decreased when warming exceeded 2???°C. The largest increase in NPP was found in regions where temperature increased by 1?¢????2???°C, and this rate of increase also contributed the most to the total increase in NPP in China's terrestrial ecosystems. Decreasing precipitation depressed the positive trend in NPP that was stimulated by warming. In northern China, warming depressed the increasing trend of NPP and warming that was accompanied by decreasing precipitation led to negative changing trends in NPP in large parts of northern China, especially when warming exceeded 2???°C. However, warming stimulated the increase in NPP until warming was greater than 2???°C, and decreased precipitation helped to increase the NPP in southern China.
机译:摘要生态系统在过去几十年中对气候变暖和相应降水变化的不同大幅度的响应可以为将来预测净初级生产力(NPP)的幅度和轨迹提供重要参考。在这项研究中,基于过程的生态系统模型,植被,土壤和大气(CEVSA)之间的碳交换,用于调查NPP在1961年期间在国家和次区域尺度的变暖的反应?¢???? 2010。结果表明,在过去50年中,温度增加了1.3 ???°C温度刺激了国家规模的正常变化趋势。无论温度升高,温暖增强了NPP的增加;然而,当变暖超过2时,NPP的正趋势降低了2 ???°C。在温度增加1的地区发现了NPP的最大增加,其中2 ???? 2 ???°C,这种增加速度也为中国陆地生态系统中NPP的总增加作出了贡献。降水降低抑制了通过变暖刺激的NPP中的正趋势。在中国北方,变暖抑制了NPP和升温的越来越大的趋势,伴随着降水降低导致中国北部大部分地区NPP的负不断变化趋势,特别是当变暖超过2 ???°C。然而,升温刺激NPP的增加,直到变暖大于2 ???°C,并且降低降水有助于增加中国南部的NPP。

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