环境C卫星热系统设计与在轨验证

根据环境C卫星的自身特性, 采用以被动式热控制为主和主动热控制为辅的控制方式, 对环境C卫星进行热系统设计. 通过研究环境C卫星的热控设计原则、热设计状态及已解决的关键问题, 对其在轨飞行温度数据进行了分析. 在轨飞行遥测结果表明, 环境C卫星热控系统方案合理, 工作稳定, 性能良好. 星上设备温度环境很好地满足了设计要求.     

光学采样成像系统传递函数补偿的试验研究

简要介绍了传递函数补偿(MTFC)验证试验,通过物理仿真和基于ISO20462的最小可觉差(JND)主观评价,对光学采样成像系统MTFC进行了研究。在实验室建立模拟采样成像系统进行物理仿真;通过对7次JND评价数据之间的相互验证,说明JND主观评价具有客观性,试验数据和MTFC验证结论准确可信。     

Altimetry,bathymetry and geoid variations at the Gavdos permanent Cal/Val facility

The aim of this work has been to examine the relationship of steep bathymetry in the coastal areas around the permanent Cal/Val facility of Gavdos, and their influence on the produced calibration values for the Jason-2 satellite altimeter. The paper describes how changes in seafloor topography (from 200 to 3500 m depth over a distance of 10 km) are reflected on the determined altimeter parameters using different reference surfaces for satellite calibration. Finally, it describes the relation between these parameter trends and the region’s local characteristics.     

Towards validation of SCIAMACHY lunar occultation NO2 vertical profiles

Vertical profiles of stratospheric nitrogen dioxide (NO₂) have been retrieved from moderate resolution lunar occultation transmission spectra measured by Scanning Imaging Absorption spectroMeter for Atmospheric CHartographY (SCIAMACHY) on board the European Environmental Satellite (ENVISAT). These measurements were taken over the high southern latitude of 50°–90° during the period of 2003–2005. To assess the accuracy of the retrieved NO₂ profiles, the SCIAMACHY nighttime NO₂ profiles were compared with NO₂ profiles retrieved from sunrise solar occultation spectra measured by the Halogen Occultation Experiment (HALOE) and the Stratospheric Aerosol and Gas Experiments II (SAGE II) using a photochemical correction model. The validation results show good agreement of SCIAMACHY lunar occultation NO₂ with scaled HALOE and SAGE II profiles. The relative mean differences (rmd) with scaled HALOE profiles are within −13% to +5% and standard deviations (rms) of the relative differences are within 3–19% between 25 and 38 km. The rmd and rms with scaled SAGE II NO₂ profiles are in the range of −9 to +7 and 10–17% respectively between 22 and 39 km.     

珠海一号高光谱卫星辐射精度真实性检验研究

“珠海一号（OHS）”高光谱商业遥感卫星数据在国民经济建设中发挥着越来越重要的作用。当前，针对商业遥感卫星数据质量精度的验证和评价研究成果较少。本文基于地面实测数据，对OHS卫星高光谱数据的辐射精度进行了真实性检验和定量分析。结果表明：OHS卫星表观辐亮度与实测结果具有较好的线性相关关系，相关系数R²大于0.7。与实测结果相比，OHS卫星各通道表观辐亮度值整体偏低，但两者光谱曲线形态基本一致。随着时间的推移，OHS传感器性能可能存在衰减，不同通道的衰减程度不一；在31个通道中，与实测值之间的相对差异在20%以内的通道数为9个；在20%~30%之间为14个，30%~40%为8个。     

Comparative evaluation of five global gravity models over a part of the Bay of Bengal

Several global gravity models (GGMs) are freely available in the public domain, which can be utilised to study the earth's gravity field in almost every part of the globe. The present study compared the free-air gravity anomalies calculated from the five GGMs EGM2008, EIGEN6C4, GECO, XGM2019e_2159, and SGG-UGM-2 archived by the International Centre for Global Earth Models (ICGEM) with respect to shipborne gravity in the Bay of Bengal. The average correlation coefficient and covariance are ～ 96 % and ～ 450mGal². The mean difference between the shipborne and the modelled gravity is ? 5 mGal. Relatively higher amplitude gravity differences observed at the continental-oceanic transition, the 85°E and Ninetyeast ridges, and the western basin are possibly due to high gradient, dominant density contrasts, and rugged topography. The average standard deviation and root-mean-square-error (RMSE) of the differences are ～ 6.5 mGal and ～ 7.5 mGal. A significantly lower standard deviation and RMSE found for the models generated at higher degree/order compared to lower degree/order is due to diminishing omission error of the GGMs with increasing degrees of truncation. The spectral analysis and coherence estimation of the modelled gravity demonstrate excellent correspondence for anomalies wider than ～ 25 km. The agreement between anomaly amplitudes and shapes and calculated statistics indicates that the accuracy and resolution of the modelled gravity data are certainly good enough for regional-scale studies aiming to map Moho topography and mantle structures. However, the delineation of shorter wavelength features originating from the shallow-level basement/sedimentary might be uncertain and requires further validations. The present study confirms that all five models show promising results in terms of their accuracy and resolution. Moreover, the SGG-UGM-2 and XGM2019e_2159 models compare favourably with respect to the GECO, EIGEN6C4 and EGM2008 models in the Bay of Bengal.     

有限元仿真模型V&V技术研究

仿真模型建模过程存在多种误差输入，将引起仿真预测结果的不精确性。采用仿真模型V&V（Verification and Validation,验证与确认）技术，进行仿真模型的建模误差分析与控制。利用物理试验数据进行仿真模型的精度评估，基于模型修正算法进行仿真建模参数的自动修正，提升仿真和试验结果的一致性，帮助设计师基于精确的仿真模型进行产品的虚拟性能预示，提升仿真技术在产品研制流程中的地位和作用。阐述了模型V&V的概念和流程，对模型V&V的关键技术和原理进行了详细论述,以NASA Rotor37转子验模为例进行了V&V案例说明。