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全球植被与大气之间碳通量的模式估计(英文)
引用本文:李银鹏 ,季劲钩.全球植被与大气之间碳通量的模式估计(英文)[J].大气科学进展,2001(5).
作者姓名:李银鹏  季劲钩
作者单位:Li Yinpeng and Ji Jinjun Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029
基金项目:This study was supported by National Key Basic Research Development Program (G1999043400).
摘    要:用大气植被相互作用模式(AVIM)模拟了全球陆地植被的净初级生产力(NPP)。AVIM由相互耦合的两部分组成:物理过程,包括陆地表面水分和能量在土壤、植被与大气之间的传输;以及生理生态过程,如:光合、呼吸、干物质分配、凋落和物候等。全球的植被分为13类,土壤按质地分为6类。用EMDI提供的全球1637个包括不同植被类型的NPP观测点数据对模型进行了检验。NPP模拟的结果表明:全球陆地植被的平均NPP为405.13gCm-2yr-1,不同植被类型的平均 NPP变化范围在99.58 g Cm-2yr-1(苔原)到996.2 g Cm-2yr-1(热带雨林)之间。全球年总NPP为60.72GtCyr-1,其中最大的部分为热带雨林,15.84GtCyr-1,占全球的26.09%。最大的碳汇是在北半球的温带。模式模拟的NPP在全球的空间和季节分布是合理的。

关 键 词:碳通量  净初级生产力(NPP)  陆地生态系统  大气植被相互作用

Model Estimates of Global Carbon Flux between Vegetation and the Atmospherer
Li Yinpeng and Ji Jinjun Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing.Model Estimates of Global Carbon Flux between Vegetation and the Atmospherer[J].Advances in Atmospheric Sciences,2001(5).
Authors:Li Yinpeng and Ji Jinjun Institute of Atmospheric Physics  Chinese Academy of Sciences  Beijing
Institution:Li Yinpeng and Ji Jinjun Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029
Abstract:The net primary productivity (NPP) of global terrestrial vegetation is estimated by an Atmosphere-Vegetation Interaction Model (AVIM). AVIM consists of two intercoupled components: phys- ical processes, involving water and energy transfer among soil vegetation and the atmosphere at the land surface and eco-physiological processes, i.e. photosynthesis, respiration, dry matter allocation, littering, phenology Globally vegetation is classificd into 13 types and soil texture is classified into 6 types. The esti- mated NPP for different vegetation types at 1637 sites are validated with the observed data provided by EMDI. The main results of NPP estimation show that global averaged NPP is 405. 13 g C m-2yr-1, varying from 99.58 g C m-2yr-1 (tundra) to 996.2 g m-2yr-1 (rainforest). Global total annual NPP is about 60.72Gt C yr-1, in which the maximum part, about 15.84 Gt C yr-1, accounting for 26.09% of the total is contributed by tropical rainforest. The maximum carbon sink occurs in the temperate region of the Northern Hemi- sphere The global spatial and seasonal distribution of terrestrial NPP is estimated reasonably.
Keywords:Carbon flux  Net primary productivity (NPP)  Terrestrial ecosystem  Atmosphere- vegetation interaction  
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