Relationship between daily variation of cosmogenic nuclide Be-7 concentration in atmosphere and solar activities

Daily Be-7 concentrations in air at the height of 15 m are continuously observed at 38°15.2′N, 140°20.9′E, between 2000 and 2001. The average concentration and the relative standard deviation were 4.0 mBq/m³ and 50% in 2000–2001, respectively. The Be-7 concentrations increased 2.5% with the decrease in the sunspot numbers by 6.7% for the term of two years. From the power spectral analysis, the periodicity of 26 days is shown for the daily Be-7 concentrations. The folding analysis indicates that the time variation of the Be-7 concentration is similar to that of the ground-based neutron counting rate, and the phase delay for the minimum portion of Be-7 concentration was roughly 8 days to the maximum sunspot number. These results indicate that the Be-7 concentrations in the air at ground level have 26 day periodicity as a component of time variations and the time variation is caused by the solar modulation of galactic cosmic rays, which corresponds to the variation of the sunspot number due to the rotation of the sun.     

J2项和大气阻力摄动作用下卫星编队构型的演化分析

研究卫星编队构型在J2项摄动和大气阻力摄动作用下的演化进程。从相对运动动力学模型出发,分别加入J2项摄动和大气阻力摄动因素,采用数值积分对所获得的运动方程求解,得到参考星和环绕星在惯性坐标系中的绝对运动规律;将两星的绝对运动规律作差后,利用坐标转换矩阵,将惯性坐标系中两星的相对运动规律转换到Hill坐标系中。由于该方法没有经过任何简化,故研究摄动的影响时不存在误差。最后通过仿真分析,给出了J2项摄动和大气阻力摄动作用下卫星编队构型演化的相关结论,并提出进一步研究的方向。     

基于大气阻力的卫星编队沿航迹方向的变结构控制

分析了大气阻力对近地轨道卫星轨道参数的影响,用变结构控制设计了基于大气阻力的编队构型沿航迹方向的控制。将中心的漂移距离和编队卫星的面质比之差作为输入量,设计滑模面进行编队控制,用极限环方式消除了在滑膜面附近的频繁切换。仿真结果验证了该控制律的正确性。     

Numerical modeling of propagation of breaking nonlinear acoustic-gravity waves from the lower to the upper atmosphere

Acoustic-gravity waves (AGWs) observed in the upper atmosphere may be generated near the Earth’s surface due to a variety of meteorological sources. Two-dimensional simulations of vertical propagation and breaking of nonlinear AGWs in the atmosphere are performed. Forcing near the Earth’s surface is used as the AGW source in the model. We use a numerical method based on finite-difference analogues of fundamental conservation laws for solving atmospheric hydrodynamic equations. This approach selects physically correct generalized solutions of the wave hydrodynamic equations. Numerical simulations are performed in a representative region of the Earth’s atmosphere up to altitude 500 km. Vertical profiles of temperature, density, molecular viscosity and heat conductivity were taken from the standard atmosphere model MSIS-90 for January. Calculations were made for different amplitudes and frequencies of lower boundary wave forcing. It is shown that after activating the tropospheric wave forcing, the initial pulse of AGWs may very quickly propagate to altitudes of 100 km and above and relatively slowly dissipate due to molecular viscosity and heat conduction. This may increase the role of transient nonstationary waves in effective energy transport and variations of atmospheric parameters and gas admixtures in a broad altitude range.     

ICCD相机遥感模型与仿真

文章介绍了一个基于增强型CCD相机 (ICCD)的遥感成像模型 ,并对模型的 4个基本组成部分 ,即ICCD相机模型、大气传输模型、地面反射率模型、星历模型 ,进行了探讨和分析 ,该模型可以模拟动态条件下 (时间、地点、气象条件等变化 )ICCD相机的成像过程。     

Spacecraft Design-for-Demise implementation strategy & decision-making methodology for low earth orbit missions

Space missions designed to completely ablate upon an uncontrolled Earth atmosphere reentry are likely to be simpler and cheaper than those designed to execute controlled reentry. This is because mission risk (unavailability) stemming from controlled reentry subsystem failure(s) is essentially eliminated. NASA has not customarily implemented Design-for-Demise meticulously. NASA has rather approached Design-for-Demise in an ad hoc manner that fails to entrench Design-for-Demise as a mission design driver. Thus, enormous demisability challenges at later formulation stages of missions aspired to be demisable are evident due to these perpetuated oversights in entrenching Design-for-Demise practices. The investigators hence propose a strategy for a consistent integration of Design-for-Demise practices in all phases of a space mission lifecycle. Secondly, an all-inclusive risk-informed, decision-making methodology referred to as Analytic Deliberative Process is proposed. This criterion facilitates in making a choice between an uncontrolled reentry demisable or controlled reentry. The authors finally conceive and synthesize Objectives Hierarchy, Attributes, and Quantitative Performance Measures of the Analytical Deliberative Process for a Design-for-Demise risk-informed decision-making process.     

航天器空间环境干扰力矩分析与仿真研究

针对航天器在轨运行时所受到的空间环境干扰力矩进行建模分析,并通过实时解算和矢量叠加的方式进行仿真研究,尤其对太阳光压力矩与大气阻力力矩的建模与仿真提出了新的方法,该方法通过建立光照面与迎风面的判断准则,准确地对太阳光压力矩与大气阻力力矩进行了估计。对各种空间环境干扰力矩的精确建模与仿真为航天器精确姿态控制设计及系统姿态控制方案和控制执行机构的选取提供了依据,文中提出的方法简单易用,工程实现性强,为未来的工程应用提供了一定的理论依据。     

红外辐射大气透过率的工程计算

针对现有红外辐射大气透过率经验计算公式不适用于高层大气的局限性，对其进行了重新推导并引入了高度修正，修正后的公式可用于计算任意高度路程上的大气透过率，修正所需大气光学特性参数全部可查相关手册获得。此外，还设计了适合于计算倾斜路径上大气透过率的计算流程，并给出了计算实例。     

大气重力波引起的突发钠层的模拟研究

应用钠原子和中性大气分子的质量连续性方程来模拟突发纳层（SSL），垂直风场采用接近实际大气重力波的正弦行波模式，结果较好地反映了SSL的形成过程。SSL的形成时刻在5－15min之间并可持续到30min之后，形成高度大约在90－100km之间，峰宽为0.5-2km之间，这些都与实际观测SSL的特点相符，同时还进一步地研究了当重力波参数（主要指垂直波长和周期）、风速以及常态钠层半宽度发生变化时SSL的变化趋势。     

大气阻力摄动计算方法及误差分析

探索了大气阻力摄动精密计算方法，以提高卫星空间位置的预报精度。根据大气阻力摄动的基本原理，给出两种摄动计算方法，即半分析半数值方法和数值积分方法。选用三种高层大气模型：ＣＩＲＡ－１９８６、ＣＩＲＡ－１９７２和ＤＴＭ模型，分批 太阳活动中高年水平（Ｆ１０．７取为１５０，２００，２５０）和１０％－２０％的模型误差引起卫星空间位置的误差δＰ。结果显示：（１）太阳活动Ｆ１０．７的大小对δＰ的影响明显，在同