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气候变化情景下中国天然植被净初级生产力的变化趋势

[Variation trends of natural vegetation net primary productivity in China under climate change scenario].

作者信息

Zhao Dong-sheng, Wu Shao-hong, Yin Yun-he

机构信息

Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2011 Apr;22(4):897-904.

Abstract

Based on the widely used Lund-Potsdam-Jena Dynamic Global Vegetation Model (LPJ) for climate change study, and according to the features of natural environment in China, the operation mechanism of the model was adjusted, and the parameters were modified. With the modified LPJ model and taking 1961-1990 as baseline period, the responses of natural vegetation net primary productivity (NPP) in China to climate change in 1991-2080 were simulated under the Special Report on Emissions Scenarios (SRES) B2 scenario. In 1961-1990, the total NPP of natural vegetation in China was about 3.06 Pg C a(-1); in 1961-2080, the total NPP showed a fluctuant decreasing trend, with an accelerated decreasing rate. Under the condition of slight precipitation change, the increase of mean air temperature would have definite adverse impact on the NPP. Spatially, the NPP decreased from southeast coast to northwest inland, and this pattern would have less variation under climate change. In eastern China with higher NPP, especially in Northeast China, east of North China, and Loess Plateau, the NPP would mainly have a decreasing trend; while in western China with lower NPP, especially in the Tibetan Plateau and Tarim Basin, the NPP would be increased. With the intensive climate change, such a variation trend of NPP would be more obvious.

摘要

基于广泛用于气候变化研究的伦德 - 波茨坦 - 耶拿动态全球植被模型(LPJ),并根据中国自然环境的特点,对该模型的运行机制进行了调整,对参数进行了修正。利用修正后的LPJ模型,以1961 - 1990年为基准期,在排放情景特别报告(SRES)B2情景下模拟了1991 - 2080年中国天然植被净初级生产力(NPP)对气候变化的响应。1961 - 1990年,中国天然植被的总NPPPP约为3.06 Pg C a(-1);1961 - 2080年,总NPP呈波动下降趋势,且下降速率加快。在降水变化轻微的情况下,平均气温升高会对NPP产生一定的不利影响。在空间上,NPP从东南沿海向西北内陆递减,这种格局在气候变化下变化较小。在中国NPP较高的东部地区,特别是东北地区、华北东部和黄土高原,NPP主要呈下降趋势;而在NPP较低的西部地区,特别是青藏高原和塔里木盆地,NPP将增加。随着气候变化加剧,NPP的这种变化趋势将更加明显。

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