Coffel Ethan D, Horton Radley M, de Sherbinin Alex
Department of Earth & Environmental Sciences, Columbia University.
NASA Goddard Institute for Space Studies.
Environ Res Lett. 2018 Jan;13(1). doi: 10.1088/1748-9326/aaa00e. Epub 2017 Dec 22.
As a result of global increases in both temperature and specific humidity, heat stress is projected to intensify throughout the 21 century. Some of the regions most susceptible to dangerous heat and humidity combinations are also among the most densely populated. Consequently, there is the potential for widespread exposure to wet bulb temperatures that approach and in some cases exceed postulated theoretical limits of human tolerance by mid- to late-century. We project that by 2080 the relative frequency of present-day extreme wet bulb temperature events could rise by a factor of 100 - 250 (approximately double the frequency change projected for temperature alone) in the tropics and parts of the mid-latitudes, areas which are projected to contain approximately half the world's population. In addition, population exposure to wet bulb temperatures that exceed recent deadly heat waves may increase by a factor of five to ten, with 150 - 750 million person-days of exposure to wet bulb temperatures above those seen in today's most severe heat waves by 2070 - 2080. Under RCP 8.5, exposure to wet bulb temperatures above 35°C - the theoretical limit for human tolerance - could exceed a million person-days per year by 2080. Limiting emissions to follow RCP 4.5 entirely eliminates exposure to that extreme threshold. Some of the most affected regions, especially Northeast India and coastal West Africa, currently have scarce cooling infrastructure, relatively low adaptive capacity, and rapidly growing populations. In the coming decades heat stress may prove to be one of the most widely experienced and directly dangerous aspects of climate change, posing a severe threat to human health, energy infrastructure, and outdoor activities ranging from agricultural production to military training.
由于全球气温和比湿度上升,预计21世纪热应激将加剧。一些最易受危险高温与高湿度组合影响的地区也是人口最密集的地区。因此,到本世纪中叶至晚期,有可能广泛暴露于湿球温度接近甚至在某些情况下超过假定的人类耐受理论极限的环境中。我们预计,到2080年,热带地区和部分中纬度地区当今极端湿球温度事件的相对频率可能会上升100至250倍(约为仅温度变化预测频率的两倍),这些地区预计将容纳世界约一半的人口。此外,人口暴露于超过近期致命热浪的湿球温度下的情况可能会增加五至十倍,到2070年至2080年,将有1.5亿至7.5亿人日暴露于高于当今最严重热浪的湿球温度下。在代表性浓度路径8.5(RCP 8.5)情景下,到2080年,暴露于高于35°C(人类耐受理论极限)的湿球温度下的情况每年可能超过100万人日。将排放限制在遵循RCP 4.5情景下可完全消除暴露于该极端阈值环境的情况。一些受影响最严重的地区,特别是印度东北部和西非沿海地区,目前制冷基础设施匮乏,适应能力相对较低,人口增长迅速。在未来几十年,热应激可能被证明是气候变化最广泛经历且直接危险的方面之一,对人类健康、能源基础设施以及从农业生产到军事训练等户外活动构成严重威胁。