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161.
162.
N.A. Zakaria S.H.M. Yusoff N.A.M. Rizal N.S.A. Hamid M.H. Hashim Z. Mohd Radzi M.H. Jusoh A. Yoshikawa T. Uozumi S. Abe 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2021,67(7):2199-2206
MAGDAS PEN was established on 19th September 2019 as one of the MAGDAS observatory arrays located at Universiti Sains Malaysia (USM) (5.15°, 100.50°). The main objective of the MAGDAS project is to monitor global electromagnetic and the ambient plasma density in the geospace environment. This installation has contributed to a better understanding of the Sun-Earth coupling system. This paper presents the installation process of one of the MAGDAS magnetometers named YU-8 T magnetic sensor and provides a preliminary analysis of geomagnetic HDZ components amplitude-time that was observed at PEN station. A one-month HDZ-geomagnetic field data was processed from 1st November to 30th November 2019. The daily variations with a consistent pattern in delta H geomagnetic field components are observed throughout the day with eastward electric field effects that are observed during solar peak hours. The delta H-component gradually increases around 0700LT and reaches the maximum reading at 1300LT with a range of value ~ 40-70nT. The value slowly decreases that started from 1400LT until the night time. The reading during the night time shows a constant variation with magnitude varies in between ?10nT to + 10nT. The average H-component value of the night time is used as the baseline for the observation system. Overall, the observed trends portray a good sign of solar quiet field and Sq with no solar-terrestrial disturbances. 相似文献
163.
V.V. Kalegaev N.A. Vlasova 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2011
Dynamical features of proton fluxes at high and middle latitudes were studied based on data measured by Sun-synchronous low-altitude (800 km height) polar-orbiting three NOAA series satellites: POES 15, 16, and 17 during the geomagnetic storm on January, 21–22, 2005. Data from three satellites that passed the Northern hemisphere along different MLTs allow reconstructing the longitudinal distribution of the proton fluxes. Measurements of protons with energies of 30–80 keV and 80–240 keV (the ring current energy range) by 0- and 90-detectors were used to evaluate and compare the longitudinal asymmetry of proton flux distribution measured in the regions equatorward and poleward of the isotropic boundary. It was found that during all the phases of the geomagnetic storm distribution of the maximum flux of precipitating protons (0-detector data) is sufficiently asymmetric. The maximal flux position along MLT is moving from pre-midnight sector in quiet time to post-midnight one before and during SSC and moving back during recovery phase. The longitudinal distribution of precipitation maxima demonstrates the local increase in afternoon sector (approximately at 13:30 MLT) and decrease in the dusk one during SSC. These features are evident consequence of the magnetosphere compression. To identify the origin of the particles, the locations of maximum fluxes have been projected to the magnetosphere. It was determined that during geomagnetic storm main and recovery phases maximum fluxes were measured at latitudes poleward of the isotropic boundary. To evaluate the trapped particle flux asymmetry, the particle fluences (90-detector data) were calculated along the satellite orbit from L = 2 to the isotropic boundary. The total fluences of trapped particles calculated along the satellite orbit show regular asymmetry between dusk and dawn during main and recovery phases. The maximal intensity of proton fluxes of both investigated populations located poleward and equatorward of the isotropic boundary is achieved during SSC. The total flux measured during crossing the anisotropic region can be considered as a proxy for ring current injection rate. 相似文献
164.
165.
分析CAPP系统在航修企业中的应用现状及存在的问题,总结航修企业工艺设计对CAPP系统提出的要求,论述开发CAPP系统的步骤和在CAPP系统开发中应注意的问题。 相似文献
166.
采用已经建立的环电流离子解析模型,结合Chamberlain地冕中性层模型,研究了2004年11月一次大磁暴期间的环电流区域中性原子(ENA)图像.结果表明,模拟的ENA图像与TC-2卫星搭载的中性原子成像仪(NUAUD)的观测图像在方位角或地方时分布、高度或纬度分布和能谱分布方面存在一定的差异.如果依据磁暴发展的不同阶段来选择环电流离子模型的方位角不对称因子和通量最大方向的方位角,增大地冕中性层在低高度区域的密度或者考虑氢(H)以外的其他中性成分,改进注入边界处的离子能谱分布函数,且考虑不同种类环电流离子的比例随磁暴发展可能发生的变化,该模型有望产生更符合观测的模拟ENA图像. 相似文献
167.
最佳轨迹地形跟随系统的预测控制 总被引:1,自引:0,他引:1
本文采用输出预测算法,为最佳轨迹地形跟随系统设计了控制器,从而简便、有效地将跟踪误差减小到一个很小的数量级,并明显缩短了轨迹重构的计算时间,给最佳轨迹地形跟随系统的实时处理带来了希望。 相似文献
168.
光磁共振测量地磁场的改进方法 总被引:3,自引:0,他引:3
根据光磁共振原理,通过光抽运,形成原子的能级分布偏极化,再加入射频信号打破塞曼能级偏极化分布,形成并输出光磁共振信号。然后,同时改变扫场和水平磁场方向,调节水平电流大小,再次获得光磁共振信号。根据2次测得的水平亥姆霍兹线圈电流,计算等效磁感强度。由仪器的垂直电流,计算地磁场垂直分量。二者合成,即可得出当地磁感强度。改进后,此方法克服了以往先测定朗德因子再测定地磁场的缺点。 相似文献
169.
陈要立 《郑州航空工业管理学院学报(管理科学版)》2004,22(1):63-66
过去,在业务的研究中,人们更多的是从业务选择来分析问题,而忽视了一个重要视角:业务本身的发展过程.从业务的三个层次:现有业务、新的业务及业务退出对企业持续成长的作用分析中,得出只有保持业务发展的三个层次协调平衡,才能实现企业持续成长的结论. 相似文献
170.
从理论上分析了CCD暗电流和光电响应不均匀性产生的原因 ,根据光电响应模型提出了CCD像素光电响应不均匀性的校正方法 ,推导出了像素光电响应不均匀性的校正系数的计算方法 ,并给出了校正性能评价方法。针对实际校正中干扰光的影响 ,提出了采用变波长去除干扰方法 ,用以对校正方法进一步修正和加强校正的稳定性。研究表明 ,能量和噪声的变化对提出的校正方法影响小 ,校正过程不受信号分布形式的影响 ,校正量对信号能量变化具有自适应性特性。仿真和实验结果验证了校正方法和校正系数算法的正确性和可行性。 相似文献