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气候变化对世界上最独特生态区的影响。

Impacts of climate change on the world's most exceptional ecoregions.

机构信息

Department of Biological Sciences, Macquarie University, Sydney, NSW 2109, Australia.

出版信息

Proc Natl Acad Sci U S A. 2011 Feb 8;108(6):2306-11. doi: 10.1073/pnas.1007217108. Epub 2011 Jan 24.

DOI:10.1073/pnas.1007217108
PMID:21262825
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3038729/
Abstract

The current rate of warming due to increases in greenhouse gas (GHG) emissions is very likely unprecedented over the last 10,000 y. Although the majority of countries have adopted the view that global warming must be limited to <2 °C, current GHG emission rates and nonagreement at Copenhagen in December 2009 increase the likelihood of this limit being exceeded by 2100. Extensive evidence has linked major changes in biological systems to 20th century warming. The "Global 200" comprises 238 ecoregions of exceptional biodiversity [Olson DM, Dinerstein E (2002) Ann Mo Bot Gard 89:199-224]. We assess the likelihood that, by 2070, these iconic ecoregions will regularly experience monthly climatic conditions that were extreme in 1961-1990. Using >600 realizations from climate model ensembles, we show that up to 86% of terrestrial and 83% of freshwater ecoregions will be exposed to average monthly temperature patterns >2 SDs (2σ) of the 1961-1990 baseline, including 82% of critically endangered ecoregions. The entire range of 89 ecoregions will experience extreme monthly temperatures with a local warming of <2 °C. Tropical and subtropical ecoregions, and mangroves, face extreme conditions earliest, some with <1 °C warming. In contrast, few ecoregions within Boreal Forests and Tundra biomes will experience such extremes this century. On average, precipitation regimes do not exceed 2σ of the baseline period, although considerable variability exists across the climate realizations. Further, the strength of the correlation between seasonal temperature and precipitation changes over numerous ecoregions. These results suggest many Global 200 ecoregions may be under substantial climatic stress by 2100.

摘要

由于温室气体(GHG)排放增加,目前的变暖速度很可能是过去 1 万年中前所未有的。尽管大多数国家都认为必须将全球变暖限制在<2°C 以内,但目前的 GHG 排放速度以及 2009 年 12 月哥本哈根会议上的分歧增加了到 2100 年这一限制被超过的可能性。大量证据表明,生物系统的重大变化与 20 世纪的变暖有关。“全球 200”包括 238 个具有特殊生物多样性的生态区[Olson DM,Dinerstein E(2002)Ann Mo Bot Gard 89:199-224]。我们评估了这些标志性生态区在 2070 年之前,每月气候条件将经常达到 1961-1990 年极端气候条件的可能性。使用气候模型集合中的>600 个实现,我们表明高达 86%的陆地和 83%的淡水生态区将经历平均每月温度模式超过 1961-1990 年基线的 2SD(2σ),包括 82%的濒危生态区。89 个生态区的整个范围都将经历极端的月平均温度,局部变暖<2°C。热带和亚热带生态区以及红树林最早面临极端条件,其中一些地区的变暖幅度<1°C。相比之下,本世纪内北方森林和苔原生物群落中的生态区很少会经历如此极端的条件。平均而言,降水模式不会超过基线期的 2σ,尽管在气候实现中存在相当大的可变性。此外,在许多生态区中,季节温度和降水变化之间的相关性很强。这些结果表明,到 2100 年,许多全球 200 生态区可能会受到相当大的气候压力。

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