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21世纪的航空与全球气候变化。

Aviation and global climate change in the 21st century.

作者信息

Lee David S, Fahey David W, Forster Piers M, Newton Peter J, Wit Ron C N, Lim Ling L, Owen Bethan, Sausen Robert

机构信息

Dalton Research Institute, Manchester Metropolitan University, John Dalton Building, Chester Street, Manchester M1 5GD, United Kingdom.

NOAA Earth System Research Laboratory, Chemical Sciences Division, Boulder, CO, USA.

出版信息

Atmos Environ (1994). 2009 Jul;43(22):3520-3537. doi: 10.1016/j.atmosenv.2009.04.024. Epub 2009 Apr 19.

Abstract

Aviation emissions contribute to the radiative forcing (RF) of climate. Of importance are emissions of carbon dioxide (CO), nitrogen oxides (NO ), aerosols and their precursors (soot and sulphate), and increased cloudiness in the form of persistent linear contrails and induced-cirrus cloudiness. The recent Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change (IPCC) quantified aviation's RF contribution for 2005 based upon 2000 operations data. Aviation has grown strongly over the past years, despite world-changing events in the early 2000s; the average annual passenger traffic growth rate was 5.3% yr between 2000 and 2007, resulting in an increase of passenger traffic of 38%. Presented here are updated values of aviation RF for 2005 based upon new operations data that show an increase in traffic of 22.5%, fuel use of 8.4% and total aviation RF of 14% (excluding induced-cirrus enhancement) over the period 2000-2005. The lack of physical process models and adequate observational data for aviation-induced cirrus effects limit confidence in quantifying their RF contribution. Total aviation RF (excluding induced cirrus) in 2005 was ∼55 mW m (23-87 mW m, 90% likelihood range), which was 3.5% (range 1.3-10%, 90% likelihood range) of total anthropogenic forcing. Including estimates for aviation-induced cirrus RF increases the total aviation RF in 2005-78 mW m (38-139 mW m, 90% likelihood range), which represents 4.9% of total anthropogenic forcing (2-14%, 90% likelihood range). Future scenarios of aviation emissions for 2050 that are consistent with IPCC SRES A1 and B2 scenario assumptions have been presented that show an increase of fuel usage by factors of 2.7-3.9 over 2000. Simplified calculations of total aviation RF in 2050 indicate increases by factors of 3.0-4.0 over the 2000 value, representing 4-4.7% of total RF (excluding induced cirrus). An examination of a range of future technological options shows that substantive reductions in aviation fuel usage are possible only with the introduction of radical technologies. Incorporation of aviation into an emissions trading system offers the potential for overall (i.e., beyond the aviation sector) CO emissions reductions. Proposals exist for introduction of such a system at a European level, but no agreement has been reached at a global level.

摘要

航空排放会影响气候的辐射强迫(RF)。重要的排放物包括二氧化碳(CO)、氮氧化物(NO )、气溶胶及其前体(烟尘和硫酸盐),以及以持久性线性凝结尾迹和诱导卷云形式增加的云量。政府间气候变化专门委员会(IPCC)最近的第四次评估报告(AR4)根据2000年的运营数据对2005年航空的辐射强迫贡献进行了量化。尽管21世纪初发生了改变世界的事件,但航空业在过去几年中仍强劲增长;2000年至2007年间,年平均客运增长率为5.3%,客运量增长了38%。这里给出的是基于新运营数据的2005年航空辐射强迫的更新值,这些数据显示在2000 - 2005年期间,交通量增加了22.5%,燃料使用量增加了8.4%,航空总辐射强迫增加了14%(不包括诱导卷云增强)。由于缺乏用于航空诱导卷云效应的物理过程模型和足够的观测数据,限制了对量化其辐射强迫贡献的信心。2005年航空总辐射强迫(不包括诱导卷云)约为55 mW/m²(23 - 87 mW/m²,90%可能性范围),占总人为强迫的3.5%(范围1.3 - 10%,90%可能性范围)。包括对航空诱导卷云辐射强迫的估计在内,2005年航空总辐射强迫增加到78 mW/m²(38 - 139 mW/m²,90%可能性范围),占总人为强迫的4.9%(2 - 14%,90%可能性范围)。已经给出了与IPCC SRES A1和B2情景假设一致的2050年航空排放未来情景,显示燃料使用量比2000年增加2.7 - 3.9倍。2050年航空总辐射强迫的简化计算表明,与2000年的值相比增加了3.0 - 4.0倍,占总辐射强迫的4 - 4.7%(不包括诱导卷云)。对一系列未来技术选项的研究表明,只有引入激进技术才有可能大幅减少航空燃料使用量。将航空纳入排放交易系统有可能实现总体(即超出航空部门)的CO₂排放减少。在欧洲层面存在引入这样一个系统的提议,但在全球层面尚未达成协议。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/451c/7185790/8bc27c6fdf77/gr1.jpg

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