在脱碳期间和之后,局地尺度持续变暖和极端事件的可能性

N. Diffenbaugh, E. Barnes, P. Keys
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引用次数: 5

摘要

虽然实现净零排放很有可能稳定长期的全球温度,但如果预期稳定全球温度也会稳定局部和区域气候,那么持续变暖和极端事件的可能性可能会导致这些努力被视为失败。利用多个全球气候模型的脱碳情景,我们发现,在实现二氧化碳净零排放后,世界大部分地区面临10年代际变暖的可能性为50%至30%,大多数地区表现出极端炎热和潮湿事件的持续可能性。此外,全球人口和国内生产总值的很大一部分可能会经历净零变暖后,包括在净零变暖后的十年里,美国、中国和印度的数亿人口和数万亿美元。这种可能性表明,一些人口最多、最富裕和最强大的地区可能会经历至少在短期内可能被认为表明气候稳定政策失败的气候条件,这突出了适应的重要性,以确保社区为脱碳期间和之后不可避免发生的气候变化做好准备。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Probability of continued local-scale warming and extreme events during and after decarbonization
Although achieving net-zero emissions is very likely to stabilize the long-term global temperature, the possibility of continued warming and extreme events could cause those efforts to be perceived as a failure if there is an expectation that stabilizing global temperature will also stabilize local and regional climate. Leveraging decarbonization scenarios from multiple global climate models, we find that much of the world faces >30% probability of decadal warming after net-zero CO2 emissions are achieved, with most areas exhibiting sustained probability of extreme hot and wet events. Further, substantial fractions of the global population and gross domestic product could experience post-net-zero warming, including hundreds of millions of people and trillions of dollars in the United States, China and India during the decade following net-zero. This likelihood suggests that some of the most populous, wealthy, and powerful regions may experience climatic conditions that could be perceived—at least in the near-term—to indicate that climate stabilization policies have failed, highlighting the importance of adaptation for ensuring that communities are prepared for the climate variations that will inevitably occur during and after decarbonization.
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