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The control of condensate in the dryer cylinders by their temperature gradient coolings

机译：通过温度梯度冷却控制干燥器缸中的冷凝物

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В.П. Сиваков; А.В. Вураско;
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1. Direct Digital Temperature, Humidity, and Condensate Control for a Dedicated Outdoor Air-Ceiling Radiant Cooling Panel System [J] . Stanley A Mumma Jae-Weon Jeong ASHRAE Transactions . 2005,第1期

机译：直接数字温度，湿度和冷凝水控制，用于专用的室外空气辐射散热面板系统
2. Direct Digital Temperature, Humidity, and Condensate Control for a Dedicated Outdoor Air-Ceiling Radiant Cooling Panel System [J] . Stanley A. Mumma, Jae-Weon Jeong ASHRAE Transactions . 2005,第Pt1期

机译：直接数字温度，湿度和冷凝水控制，用于专用的室外空气辐射散热面板系统
3. Control printing temperature with water-cooled cylinder [J] . The canmaker . 2012,第NOVa期

机译：用水冷滚筒控制打印温度
4. Expert system for the detection of condensate accumulation inside dryer cylinders during section starting [C] . Guillermo Ramirez A., Anibal Valenzuela M., Lorenz Robert.D. Annual Pulp and Paper Industry Technical Conference . 2014

机译：专家系统，用于在断面启动时检测干燥筒内部的冷凝水积聚
5. An experimental investigation of droplet impact cooling at controlled surface temperatures. [D] . Wang, Jianwei. 2000

机译：在受控的表面温度下进行液滴冲击冷却的实验研究。
6. Thermoelectrically Cooled Temperature-Gradient Apparatus for Comparative Cell and Virus Temperature Studies [O] . H. F. Clark, F. Kaminski, D. T. Karzon 1970

机译：用于比较细胞和病毒温度的热电冷却温度梯度仪
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。

The control of condensate in the dryer cylinders by their temperature gradient coolings

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