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IR-Band Conversion of Target and Background Using Surface Temperature Estimation and Error Compensation for Military IR Sensor Simulation

机译：使用表面温度估计和军用IR传感器仿真的表面温度估计和误差补偿的目标和背景的IR波段转换

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Taewuk Bae; Youngchoon Kim; Sangho Ahn;
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1. Reduction and compensation of humidity measurement errors at cold temperatures using dual QCM humidity sensors based on graphene oxides [J] . Lee Sang-Wook, Choi Byung Il, Kim Jong Chul, Sensors and Actuators . 2019,第APRa期

机译：使用基于石墨烯氧化物的双QCM湿度传感器减少和补偿寒冷温度下的湿度测量误差
2. Rapid estimation and compensation method of commutation error caused by Hall sensor installation error for BLDC motors [J] . Xuliang Yao, Chenwei Ma, Jicheng Zhao, Electric Power Applications, IET . 2020,第3期

机译：BLDC电机霍尔传感器安装误差引起的换向误差快速估计和补偿方法
3. Inverse Estimation of Surface Temperature Induced by a Moving Heat Source in a 3-D Object Based on Back Surface Temperature with Random Measurement Errors [J] . Jianhua Zhoua Yuwen Zhanga* J. K. Chena amp, Z. C. Fenga Numerical Heat Transfer, Part A: Applications . 2012,第2期

机译：基于带有随机测量误差的背面温度的3D对象中移动热源引起的表面温度的逆估计
4. Analysis of natural IR-background signatures with respect to statistical relationships between background surface temperatures and weather parameters [C] . Friedrich Theunert, German Military Geophysical Office, Traben-Trarbach, Characterization and Propagation of Sources and Backgrounds . 1994

机译：关于背景表面温度和天气参数之间的统计关系的自然红外背景特征分析
5. Accurate estimation of standard errors in the global averaging of surface temperatures. [D] . Li, Guilong. 2001

机译：精确估算表面温度的全球平均水平中的标准误差。
6. IR-Band Conversion of Target and Background Using Surface Temperature Estimation and Error Compensation for Military IR Sensor Simulation [O] . Taewuk Bae, Youngchoon Kim, Sangho Ahn 2019

机译：利用表面温度估计和误差补偿对目标和背景进行红外波段转换用于军事红外传感器仿真
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. Simulations of Strapdown-System Errors and Error Compensation Methods [R] . Wetzig, V., Zhuge, H. 1984

机译：捷联系统误差和误差补偿方法的仿真

IR-Band Conversion of Target and Background Using Surface Temperature Estimation and Error Compensation for Military IR Sensor Simulation

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