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Global Temperature Responses to Large Tropical Volcanic Eruptions in Paleo Data Assimilation Products and Climate Model Simulations Over the Last Millennium

机译：对古代数据同化产品大型热带火山爆发的全球温度应对最后一千年的气候模型模拟

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E. Tejedor; N. Steiger; J. E. Smerdon; R. Serrano‐Notivoli; M. Vuille;
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1. Northern Hemispheric cryosphere response to volcanic eruptions in the Paleoclimate Modeling Intercomparison Project 3 last millennium simulations [J] . Mira Berdahl, Alan Robock Journal of Geophysical Research, D. Atmospheres: JGR . 2013,第22期

机译：北半球冰冻圈对火山喷发的响应在古气候模拟比对项目3上一个千年模拟中
2. Effects of Large Volcanic Eruptions on Global Summer Climate and East Asian Monsoon Changes during the Last Millennium: Analysis of MPI-ESM Simulations [J] . Man WM, Zhou TJ, Jungclaus JH Journal of Climate . 2014,第19期

机译：上一个千年大火山喷发对全球夏季气候和东亚季风变化的影响：MPI-ESM模拟分析
3. Effects of Large Volcanic Eruptions on Global Summer Climate and East Asian Monsoon Changes during the Last Millennium: Analysis of MPI-ESM Simulations [J] . Man Wenmin, Zhou Tianjun, Jungclaus Johann H. Journal of Climate . 2014,第19期

机译：上一个千年大火山喷发对全球夏季气候和东亚季风变化的影响：MPI-ESM模拟分析
4. Volcanic product detection after the 2010 Merapi eruption by using VHR SAR data [C] . Bignami C., Ruch J., Chini M., IEEE International Geoscience and Remote Sensing Symposium . 2012

机译：通过使用VHR SAR数据，2010年Merapi爆发后的火山产品检测
5. Influence of volcanic eruptions on tropical hydroclimate during the last millennium [D] . Colose, Christopher M. 2017

机译：上一千年火山喷发对热带水气候的影响
6. European and Mediterranean hydroclimate responses to tropical volcanic forcing over the last millennium [O] . M. P. Rao, B. I. Cook, E. R. Cook, -1

机译：在过去的千年中欧洲和地中海的水文气候对热带火山强迫的反应
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。
8. Technical Report Series on Global Modeling and Data Assimilation, Volume 10: Dynamical Aspects of Climate Simulations Using the GEOS General Circulation Model [R] . Takacs, Lawrence L., Suarez, Max J. 1996

机译：全球建模和数据同化技术报告系列，第10卷：使用GEOs大气环流模型的气候模拟的动态方面

Global Temperature Responses to Large Tropical Volcanic Eruptions in Paleo Data Assimilation Products and Climate Model Simulations Over the Last Millennium

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