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Sea-ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate

机译：海冰诱导南海地下变暖和表面冷却在温暖的气候下

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F. Alexander Haumann; Nicolas Gruber; Matthias Münnich;
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1. The role of meltwater-induced subsurface ocean warming in regulating the Atlantic meridional overturning in glacial climate simulations [J] . Esther C. Brady, Bette L. Otto-Bliesner Climate dynamics . 2011,第7a8期

机译：融水引起的地下海洋变暖在调节冰川气候模拟中调节大西洋经向翻转中的作用
2. Sea-ice and North Atlantic climate response to CO_2-induced warming and cooling conditions [J] . Nazarenko Larissa, Tausnev Nickolai, Hansen James Journal of Glaciology . 2006,第178期

机译：海冰和北大西洋的气候对CO_2引起的变暖和变冷条件的响应
3. Subsurface ocean flywheel of coupled climate variability in the Barents Sea hotspot of global warming [J] . Pawel Schlichtholz Scientific reports. . 2019,第期

机译：耦合气候变异性的地下海洋飞轮在全球变暖的海水热点
4. ENERGY ANALYSIS OF A COMBINED HEATING AND COOLING SYSTEM FOR CONDITIONING HOTELS IN MILD AND WARM DRY CLIMATES [C] . M. De Carli, F. Cappon, L. Prendin, Sources/sinks alternative to the outside air for heat pump and air-conditioning techniques ; International sorption heat pump conference . 2011

机译：轻度和暖干气候条件下的酒店加冷空调系统的能量分析
5. Questions Raised by the Global Warming Hiatus: The Predictability of Tropical Pacific Decadal Variability and Subsurface Warming of the Tropical Atlantic Ocean [D] . Ramesh, Nandini. 2018

机译：全球变暖中断提出的问题：热带太平洋年代际变率的可预测性和热带大西洋的地下变暖
6. Change in ocean subsurface environment to suppress tropical cyclone intensification under global warming [O] . Ping Huang, I. -I Lin, Chia Chou, -1

机译：改变海洋地下环境以抑制全球变暖下的热带气旋加剧
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. Numerical Study of the Response of the Southern Ocean and Its Sea Ice to a CO2-Induced Atmospheric Warming [R] . van Ypersele, J. P. 1986

机译：南大洋及其海冰对CO2诱导的大气变暖响应的数值研究

Sea-ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate

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