Joint Global Change Research Institute, Pacific Northwest National Laboratory, College Park, MD 20740, USA.
Proc Natl Acad Sci U S A. 2013 Aug 27;110(35):14202-6. doi: 10.1073/pnas.1308470110. Epub 2013 Aug 12.
Emissions reductions focused on anthropogenic climate-forcing agents with relatively short atmospheric lifetimes, such as methane (CH4) and black carbon, have been suggested as a strategy to reduce the rate of climate change over the next several decades. We find that reductions of methane and black carbon would likely have only a modest impact on near-term global climate warming. Even with maximally feasible reductions phased in from 2015 to 2035, global mean temperatures in 2050 would be reduced by 0.16 °C, with a range of 0.04-0.35 °C because of uncertainties in carbonaceous aerosol emissions and aerosol forcing per unit of emissions. The high end of this range is only possible if total historical aerosol forcing is relatively small. More realistic emission reductions would likely provide an even smaller climate benefit. We find that the climate benefit from reductions in short-lived forcing agents are smaller than previously estimated. These near-term climate benefits of targeted reductions in short-lived forcers are not substantially different in magnitude from the benefits from a comprehensive climate policy.
减排重点放在人为气候强迫因素上,这些因素在大气中的寿命相对较短,例如甲烷(CH4)和黑碳,这被认为是在未来几十年内减缓气候变化速度的一种策略。我们发现,甲烷和黑碳的减排可能只会对近期全球气候变暖产生适度影响。即使从 2015 年到 2035 年逐步实现最大可行减排,到 2050 年,全球平均气温也只会降低 0.16°C,范围在 0.04°C 到 0.35°C 之间,这是由于碳质气溶胶排放和每单位排放的气溶胶强迫不确定性造成的。如果总历史气溶胶强迫相对较小,则可能达到该范围的高端。更现实的减排措施可能会带来更小的气候效益。我们发现,短期气候强迫因素减排带来的气候效益小于先前的估计。从短期气候强迫因素减排中获得的近期气候效益,在规模上与全面气候政策的效益没有显著区别。