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陆地生态系统对气候的影响。

The influence of terrestrial ecosystems on climate.

作者信息

Meir Patrick, Cox Peter, Grace John

机构信息

School of Geosciences, University of Edinburgh, Edinburgh EH8 9XP, UK.

出版信息

Trends Ecol Evol. 2006 May;21(5):254-60. doi: 10.1016/j.tree.2006.03.005. Epub 2006 Mar 29.

Abstract

Terrestrial ecosystems influence climate by affecting how much solar energy is absorbed by the land surface and by exchanging climatically important gases with the atmosphere. Recent model analyses show widespread qualitative agreement that terrestrial ecological processes will have a net positive feedback effect on 21st-century global warming, and, therefore, cannot be ignored in climate-change projections. However, the quantitative uncertainty in the net feedback is large. The uncertainty in 21st-century carbon dioxide emissions resulting from terrestrial carbon cycle-climate feedbacks is second in magnitude only to the uncertainty in anthropogenic emissions. We estimate that this translates into an uncertainty in global warming owing to the land surface of 1.5 degrees C by 2100. We also emphasise the need to improve our understanding of terrestrial ecological processes that influence land-atmosphere interactions at relatively long timescales (decadal-century) as well as at shorter intervals (e.g. hourly).

摘要

陆地生态系统通过影响陆地表面吸收的太阳能量以及与大气交换对气候具有重要意义的气体来影响气候。最近的模型分析表明,广泛存在定性共识,即陆地生态过程将对21世纪的全球变暖产生净正反馈效应,因此在气候变化预测中不能被忽视。然而,净反馈的定量不确定性很大。陆地碳循环 - 气候反馈导致的21世纪二氧化碳排放的不确定性在量级上仅次于人为排放的不确定性。我们估计,到2100年,这将转化为由于陆地表面导致的全球变暖的不确定性为1.5摄氏度。我们还强调,需要更好地理解在相对较长时间尺度(十年至百年)以及较短时间间隔(例如每小时)影响陆地 - 大气相互作用的陆地生态过程。

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