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Delineation of thermodynamic and dynamic responses to sea surface temperature forcing associated with El Niño

机译：与ElNiño相关的海表面温度强制划分热力学和动力响应

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Xiaoming Hu; Ming Cai; Song Yang; Zhaohua Wu;
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1. Delineation of thermodynamic and dynamic responses to sea surface temperature forcing associated with El Nino [J] . Hu Xiaoming, Cai Ming, Yang Song, Climate dynamics . 2018,第11a12期

机译：描绘与厄尔尼诺现象有关的对海面温度强迫的热力学和动力学响应
2. Seasonally Different Response of the Indian Ocean to the Remote Forcing of El Niño: Linking the Dynamics and Thermodynamics [J] . Hiroaki Ueda, Masamichi Ohba SOLA: Scientific Online Letters on the Atmosphere . 2009,第2期

机译：印度洋对厄尔尼诺现象的远程强迫的季节性不同响应：将动力学和热力学联系起来
3. Experimental and thermodynamic study of nickel-based alloys containing chromium carbides, Part II: Study of the sub-surface characteristics of Ni–30 wt% Cr–xC alloys oxidized at high temperature using thermodynamic calculations [J] . P. Berthod Calphad: Computer Coupling of Phase Diagrams and Thermochemistry . 2008,第3期

机译：含碳化铬的镍基合金的实验和热力学研究，第二部分：使用热力学计算研究高温下氧化的Ni–30 wt％Cr–xC合金的亚表面特征
4. Atomic diffusion and its relation to thermodynamic forces in Al-Ni melts [C] . Axel Griesche, Bo Zhang, Juergen Horbach, International conference on diffusion in materials . 2009

机译：原子扩散及其与Al-Ni Melts热力学力的关系
5. Atmospheric response to orbital forcing and 20th century sea surface temperatures [D] . Mantsis, Damianos F. 2011

机译：对轨道强迫和20世纪海面温度的大气反应
6. Surface Interface and Temperature Effects on the Phase Separation and Nanoparticle Self Assembly of Bi-Metallic Ni0.5Ag0.5: A Molecular Dynamics Study [O] . Ryan H. Allaire, Abhijeet Dhakane, Reece Emery, 2019

机译：表面界面和温度对双金属Ni0.5Ag0.5相分离和纳米粒子自组装的影响：分子动力学研究
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. Responses of Sea Surface Temperature and Sea Level to Wind Forcing in the Tropical Pacific [R] . Timothy, W., Tang, Wenqing 1996

机译：热带太平洋海温与海平面对风力的响应

Delineation of thermodynamic and dynamic responses to sea surface temperature forcing associated with El Niño

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