...
首页> 外文期刊>Atmosphere >The Influence of Stratospheric Sulphate Aerosol Deployment on the Surface Air Temperature and the Risk of an Abrupt Global Warming
【24h】

The Influence of Stratospheric Sulphate Aerosol Deployment on the Surface Air Temperature and the Risk of an Abrupt Global Warming

机译:平流层硫酸盐气溶胶的部署对地表气温和突然变暖风险的影响

获取原文

摘要

We used the ‘Radiative-Convective Model of the Earth-atmosphere system’ (OGIM) to investigate the cooling effects induced by sulphur injections into the stratosphere. The ensemble of numerical calculations was based on the A1B scenario from the IPCC Special Report on Emissions Scenarios (SRES). Several geoengineered scenarios were analysed, including the abrupt interruption of these injections in different scenarios and at different dates. We focused on the surface air temperature (SAT) anomalies induced by stratospheric sulphate aerosol generated in order to compensate future warming. Results show that continuous deployment of sulphur into the stratosphere could induce a lasting decrease in SAT. Retaining a constant aerosol loading equivalent to 6 TgS would delay the expected global warming by 53 years. Keeping the SAT constant in a context of increasing greenhouse gases (GHGs) means that the aerosol loading needs to be increased by 1.9% annually. This would offset the effect of increasing GHG under the A1B scenario. A major focus of this study was on the heating rates of SAT that would arise in different scenarios in case of an abrupt cessation of sulphur injections into the stratosphere. Our model results show that heating rates after geoengineering interruption would be 15–28 times higher than in a case without geoengineering, with likely important consequences for life on Earth. Larger initial sulphate loadings induced more intense warming rates when the geoengineering was stopped at the same time. This implies that, if sulphate loading was increased to maintain constant SAT in the light of increasing GHG concentrations, the later the geoengineering interruption was to occur, the higher the heating rates would be. Consequently, geoengineering techniques like this should only be regarded as last-resort measures and require intense further research should they ever become necessary.
机译:我们使用“地球大气系统的辐射对流模型”(OGIM)研究了注入平流层中的硫所引起的冷却效果。数值计算的集合是基于IPCC排放情景特别报告(SRES)中的A1B情景。分析了几种地球工程方案,包括在不同方案和不同日期突然中断这些注入。我们着重研究了平流层硫酸盐气溶胶引起的地表气温异常,以补偿未来的变暖。结果表明,硫持续向平流层中扩散会导致SAT持续降低。保持相当于6 TgS的恒定气溶胶负荷将使全球变暖的预期时间延迟53年。在温室气体(GHG)不断增加的情况下保持SAT不变意味着气溶胶负荷每年需要增加1.9%。这将抵消A1B情景下温室气体增加的影响。这项研究的主要重点是在突然停止向平流层注入硫的情况下,在不同情况下会出现的SAT加热速率。我们的模型结果表明,地球工程中断后的加热速率将比没有地球工程的情况高15-28倍,这可能对地球上的生命产生重要影响。当地球工程同时停止时,较大的初始硫酸盐负荷会引起更强烈的升温速率。这意味着,如果鉴于温室气体浓度的增加而增加硫酸盐负荷以维持恒定的SAT,则地球工程中断发生得越晚,加热速率就越高。因此,像这样的地球工程技术仅应被视为最后手段,并且在必要时需要进行深入的研究。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号