MacCracken Michael C
Climate Institute, Washington, DC 20036, USA.
J Air Waste Manag Assoc. 2008 Jun;58(6):735-86. doi: 10.3155/1047-3289.58.6.735.
Combustion of coal, oil, and natural gas, and to a lesser extent deforestation, land-cover change, and emissions of halocarbons and other greenhouse gases, are rapidly increasing the atmospheric concentrations of climate-warming gases. The warming of approximately 0.1-0.2 degrees C per decade that has resulted is very likely the primary cause of the increasing loss of snow cover and Arctic sea ice, of more frequent occurrence of very heavy precipitation, of rising sea level, and of shifts in the natural ranges of plants and animals. The global average temperature is already approximately 0.8 degrees C above its preindustrial level, and present atmospheric levels of greenhouse gases will contribute to further warming of 0.5-1 degrees C as equilibrium is re-established. Warming has been and will be greater in mid and high latitudes compared with low latitudes, over land compared with oceans, and at night compared with day. As emissions continue to increase, both warming and the commitment to future warming are presently increasing at a rate of approximately 0.2 degrees C per decade, with projections that the rate of warming will further increase if emission controls are not put in place. Such warming and the associated changes are likely to result in severe impacts on key societal and environmental support systems. Present estimates are that limiting the increase in global average surface temperature to no more than 2-2.5 degrees C above its 1750 value of approximately 15 degrees C will be required to avoid the most catastrophic, but certainly not all, consequences of climate change. Accomplishing this will require reducing emissions sharply by 2050 and to near zero by 2100. This can only be achieved if: (1) developed nations move rapidly to demonstrate that a modem society can function without reliance on technologies that release carbon dioxide (CO2) and other non-CO2 greenhouse gases to the atmosphere; and (2) if developing nations act in the near-term to sharply limit their non-CO2 emissions while minimizing growth in CO2 emissions, and then in the long-term join with the developed nations to reduce all emissions as cost-effective technologies are developed.
煤炭、石油和天然气的燃烧,以及程度较轻的森林砍伐、土地覆盖变化、卤代烃和其他温室气体排放,正在迅速增加大气中气候变暖气体的浓度。由此导致的每十年约0.1 - 0.2摄氏度的变暖很可能是积雪和北极海冰日益减少、极端强降水更频繁出现、海平面上升以及动植物自然分布范围发生变化的主要原因。全球平均气温已比工业化前水平高出约0.8摄氏度,当前大气中的温室气体水平将在重新建立平衡时导致进一步升温0.5 - 1摄氏度。与低纬度地区相比,中高纬度地区的变暖过去是、将来也会更大;与海洋相比,陆地的变暖更显著;与白天相比,夜间的变暖更明显。随着排放持续增加,当前变暖和未来变暖的趋势目前正以每十年约0.2摄氏度的速度上升,预计如果不实施排放控制,变暖速度将进一步加快。这种变暖和相关变化可能会对关键的社会和环境支持系统造成严重影响。目前的估计表明,要避免气候变化带来的最灾难性后果(但肯定不是所有后果),需要将全球平均地表温度的升幅限制在不超过比其1750年约15摄氏度的水平高出2 - 2.5摄氏度。要实现这一点,需要在2050年前大幅减少排放,并在2100年前接近零排放。只有在以下情况下才能实现这一目标:(1) 发达国家迅速采取行动,证明现代社会可以在不依赖向大气排放二氧化碳(CO₂)和其他非CO₂温室气体的技术的情况下运行;(2) 发展中国家在短期内大幅限制其非CO₂排放,同时尽量减少CO₂排放的增长,然后在长期内与发达国家一道,随着成本效益高的技术的开发减少所有排放。