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Mathematical Modeling of Processes Underlying the Spacecraft Surface Glow On orbital and Suborbital Flights

机译：轨道和亚轨道飞行中航天器表面辉光下的过程的数学模型

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来源
《Космические исследования》 |2000年第3期|p.268-277|共10页
作者
N. M. Kortsenstein; E. V. Samuilow; Yu. A. Plastinin;
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原文格式 PDF
正文语种 rus
中图分类航天（宇宙航行）;
关键词
mathematical modeling; soacecrafts; surface glow; orbital flights; suborbital flights;

机译：数学建模;手工艺品表面发光轨道飞行;亚轨道飞行;

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机译：从地球下面反射的位置信号的数学模型以及生态系统监控任务的地球底层和海景SAR图像
2. The physical aspects of gas dynamic and thermal physics processes mathematical modelling of descent spacecraft’s [J] . Igor Vasenin, Anatoliy Glazunov, Vladimir Shuvarikov, Thermal science . 2019,第Supplaa2期

机译：气体动力学和热物理的物理方面处理下降航天器的数学建模
3. A Taskable Space Vehicle Realizing Cost Savings by Combining Orbital and Suborbital Flight [J] . Thomas C. Co, Jonathan T. Black Aerospace Power Journal . 2011,第2期

机译：通过轨道与亚轨道飞行相结合实现成本节约的任务型航天器
4. Suborbital Flight Tests of a Robotics-based Payload for Studying on-Orbit Identification of Spacecraft Inertia Parameters [C] . Gerardo Martinez, Ou Ma, Milton Winkles, AIAA space forum . 2016

机译：基于机器人的有效载荷的亚轨道飞行测试，用于研究航天器惯性参数的在轨识别
5. Using Orbiter Spacecraft Data to Characterize Small-scale Surface Features on the Moon and Constrain Geophysical Properties of the Martian Crust [D] . French, Renee Apphia 2016

机译：利用轨道航天器数据表征月球上的小尺度表面特征并限制火星地壳的地球物理性质
6. Mathematical Estimation of the Level of Microbial Contamination on Spacecraft Surfaces by Volumetric Air Sampling [O] . G. S. Oxborrow, A. L. Roark, N. D. Fields, 1974

机译：通过体积空气采样对航天器表面微生物污染水平进行数学估算
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. Detection of Surface Glow Related to Spacecraft Glow Phenomenon [R] . Langer, W. D., Cohen, S. A., Manos, D. M., 1986

机译：与航天器发光现象有关的表面发光检测

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