Responses of terrestrial ecosystems to temperature and precipitation change: a meta‐analysis of experimental manipulation

生态系统 环境科学 陆地生态系统 降水 初级生产 生态系统呼吸 气候变化 生物量(生态学) 大气科学 全球变暖 生态学 生物 地理 地质学 气象学
作者
Zhuoting Wu,Paul Dijkstra,George W. Koch,Josep Peñuelas,Bruce A. Hungate
出处
期刊:Global Change Biology [Wiley]
卷期号:17 (2): 927-942 被引量:1303
标识
DOI:10.1111/j.1365-2486.2010.02302.x
摘要

Abstract Global mean temperature is predicted to increase by 2–7 °C and precipitation to change across the globe by the end of this century. To quantify climate effects on ecosystem processes, a number of climate change experiments have been established around the world in various ecosystems. Despite these efforts, general responses of terrestrial ecosystems to changes in temperature and precipitation, and especially to their combined effects, remain unclear. We used meta‐analysis to synthesize ecosystem‐level responses to warming, altered precipitation, and their combination. We focused on plant growth and ecosystem carbon (C) balance, including biomass, net primary production (NPP), respiration, net ecosystem exchange (NEE), and ecosystem photosynthesis, synthesizing results from 85 studies. We found that experimental warming and increased precipitation generally stimulated plant growth and ecosystem C fluxes, whereas decreased precipitation had the opposite effects. For example, warming significantly stimulated total NPP, increased ecosystem photosynthesis, and ecosystem respiration. Experimentally reduced precipitation suppressed aboveground NPP (ANPP) and NEE, whereas supplemental precipitation enhanced ANPP and NEE. Plant productivity and ecosystem C fluxes generally showed higher sensitivities to increased precipitation than to decreased precipitation. Interactive effects of warming and altered precipitation tended to be smaller than expected from additive, single‐factor effects, though low statistical power limits the strength of these conclusions. New experiments with combined temperature and precipitation manipulations are needed to conclusively determine the importance of temperature–precipitation interactions on the C balance of terrestrial ecosystems under future climate conditions.
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