Fuglestvedt J, Rogelj J, Millar R J, Allen M, Boucher O, Cain M, Forster P M, Kriegler E, Shindell D
CICERO Center for International Climate Research, PO Box 1129, Blindern, 0318 Oslo, Norway
Energy Program, International Institute for Applied Systems Analysis (IIASA), 2361 Laxenburg, Austria.
Philos Trans A Math Phys Eng Sci. 2018 May 13;376(2119). doi: 10.1098/rsta.2016.0445.
The main goal of the Paris Agreement as stated in Article 2 is 'holding the increase in the global average temperature to well below 2°C above pre-industrial levels and pursuing efforts to limit the temperature increase to 1.5°C'. Article 4 points to this long-term goal and the need to achieve 'balance between anthropogenic emissions by sources and removals by sinks of greenhouse gases'. This statement on 'greenhouse gas balance' is subject to interpretation, and clarifications are needed to make it operational for national and international climate policies. We study possible interpretations from a scientific perspective and analyse their climatic implications. We clarify how the implications for individual gases depend on the metrics used to relate them. We show that the way in which balance is interpreted, achieved and maintained influences temperature outcomes. Achieving and maintaining net-zero CO-equivalent emissions conventionally calculated using GWP (100-year global warming potential) and including substantial positive contributions from short-lived climate-forcing agents such as methane would result in a sustained decline in global temperature. A modified approach to the use of GWP (that equates constant emissions of short-lived climate forcers with zero sustained emission of CO) results in global temperatures remaining approximately constant once net-zero CO-equivalent emissions are achieved and maintained. Our paper provides policymakers with an overview of issues and choices that are important to determine which approach is most appropriate in the context of the Paris Agreement.This article is part of the theme issue 'The Paris Agreement: understanding the physical and social challenges for a warming world of 1.5°C above pre-industrial levels'.
《巴黎协定》第2条所述的主要目标是“将全球平均气温升幅控制在远低于工业化前水平2°C以内,并努力将气温升幅限制在1.5°C以内”。第4条指出了这一长期目标以及实现“温室气体源的人为排放与汇的清除之间的平衡”的必要性。关于“温室气体平衡”的这一表述有待解读,需要加以澄清以便在国家和国际气候政策中付诸实施。我们从科学角度研究可能的解读,并分析其气候影响。我们阐明了对个别气体的影响如何取决于用于关联这些气体的指标。我们表明,平衡的解读、实现和维持方式会影响温度结果。按照常规使用全球升温潜能值(100年全球变暖潜能值)计算并实现和维持净零二氧化碳当量排放,且包括甲烷等短期气候强迫因子的大量正贡献,将导致全球气温持续下降。对全球升温潜能值的一种改进用法(即将短期气候强迫因子的恒定排放等同于二氧化碳的零持续排放)会使一旦实现并维持净零二氧化碳当量排放,全球气温大致保持恒定。我们的论文为政策制定者概述了一些问题和选择,这些对于确定在《巴黎协定》背景下哪种方法最为合适很重要。本文是主题为“《巴黎协定》:理解升温至比工业化前水平高1.5°C的世界所面临的物理和社会挑战”这一特刊的一部分。