Jiu Jiang, Yi Xia, Long Cao, Ben Kravitz, Douglas G. MacMartin, Jianjie Fu, Guibin Jiang
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引用次数: 0
Abstract
Stratospheric aerosol injection (SAI) has been proposed as a potential supplement to mitigate some climate impacts of anthropogenic warming. Using Community Earth System Model ensemble simulation results, we analyze the response of temperature and precipitation extremes to two different SAI strategies: one injects SO2 at the equator to stabilize global mean temperature and the other injects SO2 at multiple locations to stabilize global mean temperature as well as the interhemispheric and equator-to-pole temperature gradients. Our analysis shows that in the late 21st century, compared with the present-day climate, both equatorial and multi-location injection lead to reduced hot extremes in the tropics, corresponding to overcooling of the mean climate state. In mid-to-high latitude regions, in comparison to the present-day climate, substantial decreases in cold extremes are observed under both equatorial and multi-location injection, corresponding to residual winter warming of the mean climate state. Both equatorial and multi-location injection reduce precipitation extremes in the tropics below the present-day level, associated with the decrease in mean precipitation. Overall, for most regions, temperature and precipitation extremes show reduced change in response to multi-location injection than to equatorial injection, corresponding to reduced mean climate change for multi-location injection. In comparison with equatorial injection, in response to multi-location injection, most land regions experience fewer years with significant change in cold extremes from the present-day level, and most tropical regions experience fewer years with significant change in hot extremes. The design of SAI strategies to mitigate anthropogenic climate extremes merits further study.
平流层气溶胶注入(SAI)被认为是缓解人为变暖对气候影响的潜在补充手段。利用共同体地球系统模式集合模拟结果,我们分析了极端温度和降水对两种不同 SAI 策略的响应:一种是在赤道注入二氧化硫以稳定全球平均温度,另一种是在多个地点注入二氧化硫以稳定全球平均温度以及半球间和赤道到极地的温度梯度。我们的分析表明,与现在的气候相比,在 21 世纪晚期,赤道和多地点注入二氧化硫都会导致热带地区的极端高温减少,相当于平均气候状态过冷。在中高纬度地区,与现在的气候相比,赤道注入和多地点注入都会导致极端寒冷现象大幅减少,这与平均气候状态的冬季残余变暖相对应。赤道和多地点注入都使热带地区的极端降水量低于现今水平,这与平均降水量的减少有关。总体而言,与赤道注入相比,大多数地区的极端气温和极端降水在多地点注入后变化较小,这与多地点注入的平均气候变化减少相对应。与赤道注水相比,在多地点注水的作用下,大多数陆地地区的极端低温发生显著变化的年份比现在少,大多数热带地区的极端高温发生显著变化的年份比现在少。设计减缓人为极端气候的 SAI 战略值得进一步研究。
期刊介绍:
Earth’s Future: A transdisciplinary open access journal, Earth’s Future focuses on the state of the Earth and the prediction of the planet’s future. By publishing peer-reviewed articles as well as editorials, essays, reviews, and commentaries, this journal will be the preeminent scholarly resource on the Anthropocene. It will also help assess the risks and opportunities associated with environmental changes and challenges.