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非洲与全球碳循环。

Africa and the global carbon cycle.

作者信息

Williams Christopher A, Hanan Niall P, Neff Jason C, Scholes Robert J, Berry Joseph A, Denning A Scott, Baker David F

机构信息

Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO 80523, USA.

出版信息

Carbon Balance Manag. 2007 Mar 7;2:3. doi: 10.1186/1750-0680-2-3.

DOI:10.1186/1750-0680-2-3
PMID:17343752
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC1821324/
Abstract

The African continent has a large and growing role in the global carbon cycle, with potentially important climate change implications. However, the sparse observation network in and around the African continent means that Africa is one of the weakest links in our understanding of the global carbon cycle. Here, we combine data from regional and global inventories as well as forward and inverse model analyses to appraise what is known about Africa's continental-scale carbon dynamics. With low fossil emissions and productivity that largely compensates respiration, land conversion is Africa's primary net carbon release, much of it through burning of forests. Savanna fire emissions, though large, represent a short-term source that is offset by ensuing regrowth. While current data suggest a near zero decadal-scale carbon balance, interannual climate fluctuations (especially drought) induce sizeable variability in net ecosystem productivity and savanna fire emissions such that Africa is a major source of interannual variability in global atmospheric CO2. Considering the continent's sizeable carbon stocks, their seemingly high vulnerability to anticipated climate and land use change, as well as growing populations and industrialization, Africa's carbon emissions and their interannual variability are likely to undergo substantial increases through the 21st century.

摘要

非洲大陆在全球碳循环中发挥着巨大且日益重要的作用,对气候变化可能产生重大影响。然而,非洲大陆及其周边稀疏的观测网络意味着,在我们对全球碳循环的认知中,非洲是最薄弱的环节之一。在此,我们结合区域和全球清单数据以及正向和反向模型分析,来评估关于非洲大陆尺度碳动态的已知情况。由于化石燃料排放较低,且生产力在很大程度上补偿了呼吸作用,土地转换是非洲主要的净碳释放途径,其中大部分是通过森林燃烧实现的。稀树草原火灾排放虽量大,但只是一个短期来源,随后的植被再生会将其抵消。虽然目前的数据表明十年尺度的碳平衡接近零,但年际气候波动(尤其是干旱)会导致净生态系统生产力和稀树草原火灾排放出现相当大的变化,以至于非洲是全球大气二氧化碳年际变化的主要来源。鉴于非洲大陆拥有可观的碳储量,它们似乎极易受到预期的气候和土地利用变化的影响,再加上人口增长和工业化进程不断加快,到21世纪,非洲的碳排放及其年际变化可能会大幅增加。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/6facb4abebfc/1750-0680-2-3-5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/a195649e38ab/1750-0680-2-3-1.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/59bd06b61705/1750-0680-2-3-3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/b8a8293738aa/1750-0680-2-3-4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/6facb4abebfc/1750-0680-2-3-5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/a195649e38ab/1750-0680-2-3-1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/1ed763a5ef0a/1750-0680-2-3-2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/59bd06b61705/1750-0680-2-3-3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/b8a8293738aa/1750-0680-2-3-4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3871/1821324/6facb4abebfc/1750-0680-2-3-5.jpg

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