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在未来气候的近未来变化下,东亚生态系统的生态生理过程和碳预算的变化:对基于过程模型的长期监测的启示。

Changing ecophysiological processes and carbon budget in East Asian ecosystems under near-future changes in climate: implications for long-term monitoring from a process-based model.

机构信息

National Institute for Environmental Studies, Onogawa 16-2, Tsukuba, Ibaraki, 305-8506, Japan.

出版信息

J Plant Res. 2010 Jul;123(4):577-88. doi: 10.1007/s10265-009-0305-x. Epub 2010 Feb 19.

Abstract

Using a process-based model, I assessed how ecophysiological processes would respond to near-future global changes predicted by coupled atmosphere-ocean climate models. An ecosystem model, Vegetation Integrative SImulator for Trace gases (VISIT), was applied to four sites in East Asia (different types of forest in Takayama, Tomakomai, and Fujiyoshida, Japan, and an Alpine grassland in Qinghai, China) where observational flux data are available for model calibration. The climate models predicted +1-3 degrees C warming and slight change in annual precipitation by 2050 as a result of an increase in atmospheric CO2. Gross primary production (GPP) was estimated to increase substantially at each site because of improved efficiency in the use of water and radiation. Although increased respiration partly offset the GPP increase, the simulation showed that these ecosystems would act as net carbon sinks independent of disturbance-induced uptake for recovery. However, the carbon budget response relied strongly on nitrogen availability, such that photosynthetic down-regulation resulting from leaf nitrogen dilution largely decreased GPP. In relation to long-term monitoring, these results indicate that the impacts of global warming may be more evident in gross fluxes (e.g., photosynthesis and respiration) than in the net CO2 budget, because changes in these fluxes offset each other.

摘要

利用一个基于过程的模型,我评估了生态生理过程将如何应对由耦合大气-海洋气候模型预测的近未来全球变化。一个生态系统模型,即痕量气体植被综合模拟器(VISIT),被应用于东亚的四个地点(日本高山市、苫小牧市和富士吉田的不同类型森林,以及中国青海的高山草原),这些地点都有可用于模型校准的观测通量数据。气候模型预测,由于大气 CO2 增加,到 2050 年,气温将升高 1-3 摄氏度,年降水量将略有变化。由于水和辐射利用效率的提高,预计每个地点的总初级生产力(GPP)都会大幅增加。尽管呼吸作用部分抵消了 GPP 的增加,但模拟表明,这些生态系统将成为独立于干扰诱导吸收的净碳汇。然而,碳预算的响应强烈依赖于氮的供应,因此叶片氮稀释导致的光合作用下调大大降低了 GPP。就长期监测而言,这些结果表明,与净 CO2 预算相比,全球变暖的影响可能在总通量(如光合作用和呼吸作用)中更为明显,因为这些通量的变化相互抵消。

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