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Assessing the controllability of Arctic sea ice extent by sulfate aerosol geoengineering

机译:用硫酸盐气溶胶地球工程技术评估北极海冰范围的可控性

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In an assessment of how Arctic sea ice cover could be remediated in a warming world, we simulated the injection of SO2 into the Arctic stratosphere making annual adjustments to injection rates. We treated one climate model realization as a surrogate "real world" with imperfect "observations" and no rerunning or reference to control simulations. SO2 injection rates were proposed using a novel model predictive control regime which incorporated a second simpler climate model to forecast "optimal" decision pathways. Commencing the simulation in 2018, Arctic sea ice cover was remediated by 2043 and maintained until solar geoengineering was terminated. We found quantifying climate side effects problematic because internal climate variability hampered detection of regional climate changes beyond the Arctic. Nevertheless, through decision maker learning and the accumulation of at least 10 years time series data exploited through an annual review cycle, uncertainties in observations and forcings were successfully managed.
机译:在评估如何在变暖的世界中纠正北极海冰盖的过程中,我们模拟了向北极平流层注入SO2并逐年调整注入速率的情况。我们将一种气候模型实现视为具有“不完美”“观察”的替代“现实世界”,没有重新运行或引用控制模拟。使用新颖的模型预测控制机制提出了SO2注入速率,该模型结合了第二个更简单的气候模型来预测“最佳”决策途径。从2018年开始进行模拟,到2043年,北极海冰覆盖层得到修复,一直保持到太阳能地球工程终止。我们发现量化气候副作用是有问题的,因为内部气候变异性阻碍了对北极以外区域气候变化的探测。尽管如此,通过决策者的学习和至少10年的时间序列数据的积累(通过年度审查周期),成功地管理了观测和强迫方面的不确定性。

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