中国陆地生态系统净初级生产模拟

H. Yong, Dan Li, Dong Wen-jie, Jiagn Jin-jun
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引用次数: 14

摘要

本文利用在区域和全球尺度上均得到验证的大气—植被相互作用模型(AVIM)估算了中国现代陆地生态系统净初级生产力(NPP)变化及其对气候变化的响应。AVIM由物理过程和生态生理过程两个相互耦合的部分组成,涉及大气、植被和土壤之间的物质和能量平衡。中国植被分为9种类型,土壤质地分为6种类型。收集了不同植被类型的生态生理过程参数。作为模式强迫的0.5×0.5网格单元的每日天气数据来自英国东安格利亚大学气候研究部门的月度气候数据。中国植被NPP估算值在0 ~ 1 389 gC/(cm~2·a)之间变化,平均为355 gC/(cm~2·a)。热带雨林植被的NPP值较高,无覆盖灌木的NPP值较低。NPP自东向西递减,云南南部地区NPP最高,西藏和新疆地区最低。陆地生态系统的总NPP为(3.33)Pg C,表明中国植被从大气中吸收了这么多的碳。研究还表明,降水是影响中国陆地生态系统NPP的主要因素。
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THE NET PRIMARY PRODUCTION SIMULATION OF TERRESTRIAL ECOSYSTEMS IN CHINA BY AVIM
In this paper we used an Atmosphere-Vegetation Interaction Model (AVIM) that has been validated at regional and global scales to estimate the NPP (net primary production) variation of modern Chinese terrestrial ecosystems and its responses to the climate change. AVIM consists of two inter-coupled components: physical process and eco-physiological process, involving the mater and energy balance between the atmosphere, vegetation and soil. Chinese vegetation is classified 9 types and soil texture is classified into 6 types. The parameters of eco-physiological processes for each vegetation type for AVIM are collected. Daily weather data for 0.5×0.5 grid cells as the forcing of the model are generated from the monthly climate data, coming from the climate research unit, University of East Anglia, UK. The estimated NPP of chinese vegetation changes from 0 to 1 389 gC/(cm~2·a), averaging 355 gC/(cm~2·a). Vegetation from the rain forest has the high NPP value, and the low NPP corresponding to the shrub with no cover. The NPP decreases from east to west in China, with the highest NPP occuring at the south area of Yunnan Province, and the lowest appearing at Tibet and Xinjiang areas. Total NPP of the terrestrial ecosystems is (3.33) Pg C, suggesting that such amount of carbon is absorbed from the atmosphere by the vegetation in China. Our work also shows that precipitation is the main factor affecting the NPP of terrestrial ecosystems in China.
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