School of Earth and Ocean Sciences, University of Victoria, PO Box 3065, STN CSC, Victoria, British Columbia, Canada V8W 3V6.
Philos Trans A Math Phys Eng Sci. 2012 Sep 13;370(1974):4197-216. doi: 10.1098/rsta.2012.0004.
The ultimate climate emergency is a 'runaway greenhouse': a hot and water-vapour-rich atmosphere limits the emission of thermal radiation to space, causing runaway warming. Warming ceases only after the surface reaches approximately 1400 K and emits radiation in the near-infrared, where water is not a good greenhouse gas. This would evaporate the entire ocean and exterminate all planetary life. Venus experienced a runaway greenhouse in the past, and we expect that the Earth will in around 2 billion years as solar luminosity increases. But could we bring on such a catastrophe prematurely, by our current climate-altering activities? Here, we review what is known about the runaway greenhouse to answer this question, describing the various limits on outgoing radiation and how climate will evolve between these. The good news is that almost all lines of evidence lead us to believe that is unlikely to be possible, even in principle, to trigger full a runaway greenhouse by addition of non-condensible greenhouse gases such as carbon dioxide to the atmosphere. However, our understanding of the dynamics, thermodynamics, radiative transfer and cloud physics of hot and steamy atmospheres is weak. We cannot therefore completely rule out the possibility that human actions might cause a transition, if not to full runaway, then at least to a much warmer climate state than the present one. High climate sensitivity might provide a warning. If we, or more likely our remote descendants, are threatened with a runaway greenhouse, then geoengineering to reflect sunlight might be life's only hope. Injecting reflective aerosols into the stratosphere would be too short-lived, and even sunshades in space might require excessive maintenance. In the distant future, modifying Earth's orbit might provide a sustainable solution. The runaway greenhouse also remains relevant in planetary sciences and astrobiology: as extrasolar planets smaller and nearer to their stars are detected, some will be in a runaway greenhouse state.
终极气候紧急情况是“失控的温室效应”:一个炎热且富含水蒸气的大气层限制了热辐射向太空的排放,导致失控的变暖。只有当表面温度达到约 1400K 并在近红外辐射中发射辐射时,变暖才会停止,而在近红外辐射中,水蒸气不是一种良好的温室气体。这将蒸发整个海洋并消灭所有行星生命。金星过去曾经历过失控的温室效应,我们预计随着太阳亮度的增加,地球将在大约 20 亿年后也会经历这种情况。但是,我们目前改变气候的活动是否会过早地引发这样的灾难呢?在这里,我们回顾了关于失控温室效应的已知知识,以回答这个问题,描述了限制向外辐射的各种因素以及气候在这些因素之间的演变。好消息是,几乎所有的证据都表明,即使从理论上讲,通过向大气中添加不可冷凝的温室气体(如二氧化碳)来引发完全失控的温室效应也是不太可能的。然而,我们对炎热和潮湿大气的动力学、热力学、辐射传输和云物理学的理解还很薄弱。因此,我们不能完全排除人类活动可能导致过渡的可能性,如果不是完全失控,那么至少会导致比现在更温暖的气候状态。高气候敏感性可能会提供一个警告。如果我们,或者更有可能是我们的遥远后代,面临失控的温室效应的威胁,那么反射阳光的地球工程可能是生命的唯一希望。向平流层注入反射气溶胶的时间太短,即使在太空中设置遮阳板也可能需要过度的维护。在遥远的未来,改变地球的轨道可能提供一种可持续的解决方案。失控的温室效应在行星科学和天体生物学中仍然具有相关性:随着越来越小且更接近恒星的系外行星被探测到,其中一些将处于失控的温室效应状态。