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Modeling responses of the meadow steppe dominated by Leymus chinensis to climate change

机译:羊草为主的草甸草原对气候变化的模拟响应

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摘要

Grassland is one of the most widespread vegetation types worldwide and plays a significant role in regional climate and global carbon cycling. Understanding the sensitivity of Chinese grassland ecosystems to climate change and elevated atmospheric CO2 and the effect of these changes on the grassland ecosystems is a key issue in global carbon cycling. China encompasses vast grassland areas of 354 million ha of 17 major grassland types, according to a national grassland survey. In this study, a process-based terrestrial model the CENTURY model was used to simulate potential changes in net primary productivity (NPP) and soil organic carbon (SOC) of the Leymus chinensis meadow steppe (LCMS) under different scenarios of climatic change and elevated atmospheric CO2. The LCMS sensitivities, its potential responses to climate change, and the change in capacity of carbon stock and sequestration in the future are evaluated. The results showed that the LCMS NPP and SOC are sensitive to climatic change and elevated CO2. In the next 100 years, with doubled CO2 concentration, if temperature increases from 2.7-3.9?C and precipitation increases by 10% NPP and SOC will increase by 7-21% and 5-6% respectively. However, if temperature increases by 7.5-7.8?C and precipitation increases by only 10% NPP and SOC would decrease by 24% and 8% respectively. Therefore, changes in the NPP and SOC of the meadow steppe are attributed mainly to the amount of temperature and precipitation change and the atmospheric CO2 concentration in the future.
机译:草原是全球最广泛的植被类型之一,在区域气候和全球碳循环中发挥着重要作用。了解中国草地生态系统对气候变化和大气CO2浓度升高的敏感性以及这些变化对草地生态系统的影响是全球碳循环的关键问题。根据一项全国性的草原调查,中国的草原面积达3.54亿公顷,涵盖17种主要草原类型。在这项研究中,使用基于过程的地面模型CENTURY模型来模拟在气候变化和高海拔不同情景下羊草草甸草原(LCMS)的净初级生产力(NPP)和土壤有机碳(SOC)的潜在变化大气中的二氧化碳。评估了LCMS的敏感性,其对气候变化的潜在响应以及未来碳储量和封存量的变化。结果表明,LCMS NPP和SOC对气候变化和CO2升高敏感。在接下来的100年中,如果CO2浓度增加一倍,如果温度从2.7-3.9°C升高并且降水量增加10%,那么NPP和SOC将分别增加7-21%和5-6%。但是,如果温度升高7.5-7.8?C,而降水量仅增加10%,则NPP和SOC分别降低24%和8%。因此,草甸草原NPP和SOC的变化主要归因于未来温度和降水量的变化以及大气CO2的浓度。

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  • 来源
    《Climatic Change》 |2007年第4期|437-452|共16页
  • 作者单位

    Laboratory of Quantitative Vegetation Ecology Institute of Botany The Chinese Academy of Sciences Beijing 100093 China;

    Laboratory of Quantitative Vegetation Ecology Institute of Botany The Chinese Academy of Sciences Beijing 100093 China;

    Canadian Forest Service Northern Forestry Centre 5320-122 St. Edmonton AB Canada T6H3S5;

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