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Comparison of Four Models of Radiative Heat Transfer Between Flat Surface to Evaluate the Temperature Field Based on Example of the Continuous Casting Mould

机译：作者：张莹莹，王汝传，闫澍旺，模具工

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Rywotycki M.; Malinowski Z.; Miłkowska-Piszczek K.; Gołdasz A.; Hadała B.;
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1. COMPARISON OF FOUR MODELS OF RADIATIVE HEAT TRANSFER BETWEEN FLAT SURFACE TO EVALUATE THE TEMPERATURE FIELD BASED ON EXAMPLE OF THE CONTINUOUS CASTING MOULD [J] . Rywotycki M., Malinowski Z., Milkowska-Piszczek K., Archives of Metallurgy and Materials . 2015,第1期

机译：基于连铸模具实例的平板表面辐射传热的四种模型评估温度场的比较
2. Comparison of Four Models of Radiative Heat Transfer Between Flat Surface to Evaluate the Temperature Field Based on Example of the Continuous Casting Mould [J] . M. Rywotycki, Z. Malinowski, K. Mi?kowska-Piszczek, Archives of Metallurgy and Materials . 2015,第1期

机译：以连铸结晶器为例，比较四种平面之间的辐射传热模型评估温度场
3. COMPARISON OF FOUR MODELS OF RADIATIVE HEAT TRANSFER BETWEEN FLAT SURFACE TO EVALUATE THE TEMPERATURE FIELD BASED ON EXAMPLE OF THE CONTINUOUS CASTING MOULD [J] . Rywotycki M., Malinowski Z., Milkowska-Piszczek K., Archives of Metallurgy and Materials . 2015,第1期

机译：基于连续铸模的例子，对平面辐射传热的四种辐射传热型号的比较
4. EFFECTS OF CaF_2 ON THE RADIATIVE HEAT TRANSFER IN MOULD FLUXES FOR CONTINUOUS STEEL CASTING [C] . Masahiro Susa, Yuta Kono, Rie Endo, International Conference on Molten Slags, Fluxes and Salts . 2016

机译：CAF_2对连续钢铸造模具助熔剂辐射传热的影响
5. Mould thermal response, billet surface quality and mould-flux behaviour in the continuous casting of steel billets with powder lubrication. [D] . Pinheiro, Carlos Alberto Martins. 1998

机译：采用粉末润滑的钢坯连续铸造中的结晶器热响应，钢坯表面质量和熔剂行为。
6. Surface temperatures in New York City: Geospatial data enables the accurate prediction of radiative heat transfer [O] . Masoud Ghandehari, Thorsten Emig, Milad Aghamohamadnia -1

机译：纽约市的地表温度：地理空间数据可准确预测辐射热传递
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。

Comparison of Four Models of Radiative Heat Transfer Between Flat Surface to Evaluate the Temperature Field Based on Example of the Continuous Casting Mould

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