Radiative Climate Forcing by Anthropogenic Greenhouse Gas Emissions in Finland

J. Sinisalo; I. Savolainen

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Radiative Climate Forcing by Anthropogenic Greenhouse Gas Emissions in Finland

机译：芬兰人为温室气体排放造成的辐射性气候强迫

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《Geophysica》 |1996年第3期|共12页
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J. Sinisalo; I. Savolainen;
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1. Radiative Climate Forcing by Anthropogenic Greenhouse Gas Emissions in Finland [J] . J. Sinisalo, I. Savolainen Geophysica . 1996,第1a2期

机译：芬兰人为温室气体排放造成的辐射性气候强迫
2. Radiative Forcing Due to Anthropogenic Greenhouse Gas Emissions from Finland: Methods for Estimating Forcing of a Country or an Activity [J] . SUVI MONNI, RIITTA KORHONEN, ILKKA SAVOLAINEN Environmental Management . 2003,第3期

机译：来自芬兰的人为温室气体排放所造成的辐射强迫：估算一个国家或一项活动的强迫的方法
3. Sensitivity of radiative forcing, ocean heat uptake, and climate feedback to changes in anthropogenic greenhouse gases and aerosols [J] . D. Paynter, T. L. Fr?licher Journal of Geophysical Research, D. Atmospheres: JGR . 2015,第19期

机译：辐射强迫，海洋热量吸收和气候反馈对人为温室气体和气溶胶变化的敏感性
4. An examination of anthropogenic climate forcing in the 21st century: greenhouse gases and aerosols - direct and indirect [C] . Prather, M. Geoscience and Remote Sensing Symposium, 2003. IGARSS '03. Proceedings. 2003 IEEE International . 2003

机译：对21世纪人为气候强迫的考察：温室气体和气溶胶-直接和间接
5. Impacts of anthropogenic aerosol and greenhouse gas emissions on clouds, convection, and precipitation as simulated by a super-parameterized global climate model. [D] . Kooperman, Gabriel J. 2014

机译：超参数化全球气候模型模拟的人为气溶胶和温室气体排放对云，对流和降水的影响。
6. Time-dependent climate sensitivity and the legacy of anthropogenic greenhouse gas emissions [O] . Richard E. Zeebe 2013

机译：随时间变化的气候敏感性和人为温室气体排放的影响
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. Non-CO2 Greenhouse Gas Emissions from Boilers and Industrial Processes. Evaluation and Update of Emission Factors for the Finnish National Greenhouse Gas Inventory Research note [R] . Tsupari, E. 2005

机译：锅炉和工业过程中的非CO2温室气体排放。芬兰国家温室气体清单研究报告的排放因子评估和更新

Radiative Climate Forcing by Anthropogenic Greenhouse Gas Emissions in Finland

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