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减少二氧化碳排放、二氧化碳去除和太阳辐射管理之间的相互作用。

Interactions between reducing CO2 emissions, CO2 removal and solar radiation management.

机构信息

School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK.

出版信息

Philos Trans A Math Phys Eng Sci. 2012 Sep 13;370(1974):4343-64. doi: 10.1098/rsta.2012.0188.

Abstract

We use a simple carbon cycle-climate model to investigate the interactions between a selection of idealized scenarios of mitigated carbon dioxide emissions, carbon dioxide removal (CDR) and solar radiation management (SRM). Two CO(2) emissions trajectories differ by a 15-year delay in the start of mitigation activity. SRM is modelled as a reduction in incoming solar radiation that fully compensates the radiative forcing due to changes in atmospheric CO(2) concentration. Two CDR scenarios remove 300 PgC by afforestation (added to vegetation and soil) or 1000 PgC by bioenergy with carbon capture and storage (removed from system). Our results show that delaying the start of mitigation activity could be very costly in terms of the CDR activity needed later to limit atmospheric CO(2) concentration (and corresponding global warming) to a given level. Avoiding a 15-year delay in the start of mitigation activity is more effective at reducing atmospheric CO(2) concentrations than all but the maximum type of CDR interventions. The effects of applying SRM and CDR together are additive, and this shows most clearly for atmospheric CO(2) concentration. SRM causes a significant reduction in atmospheric CO(2) concentration due to increased carbon storage by the terrestrial biosphere, especially soils. However, SRM has to be maintained for many centuries to avoid rapid increases in temperature and corresponding increases in atmospheric CO(2) concentration due to loss of carbon from the land.

摘要

我们使用一个简单的碳循环-气候模型来研究一系列经过理想化的减排、碳去除(CDR)和太阳辐射管理(SRM)情景之间的相互作用。两种二氧化碳排放轨迹的区别在于缓解活动开始时间相差 15 年。SRM 被建模为减少到达地球的太阳辐射量,该辐射量完全补偿了由于大气二氧化碳浓度变化而导致的辐射强迫。两种 CDR 情景通过造林(增加到植被和土壤中)或生物能源与碳捕获和储存(从系统中去除)来去除 3000 亿公吨碳。我们的结果表明,延迟缓解活动的开始可能会在以后需要进行碳去除活动方面付出非常高的代价,以将大气二氧化碳浓度(和相应的全球变暖)限制在给定水平。避免缓解活动开始时间延迟 15 年比除了最大类型的 CDR 干预之外的所有干预措施更能有效降低大气二氧化碳浓度。同时应用 SRM 和 CDR 的效果是相加的,这在大气二氧化碳浓度方面表现得最为明显。由于陆地生物圈,特别是土壤,储存了更多的碳,SRM 导致大气二氧化碳浓度显著降低。然而,为了避免由于陆地碳损失导致的温度迅速升高和相应的大气二氧化碳浓度增加,SRM 必须维持几个世纪。

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