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51.
航天器太阳帆板展开过程的最优控制 总被引:10,自引:0,他引:10
本文讨论航天器太阳帆板展开过程中主体姿态的最优控制问题. 利用多体动力学与最优控制理论建立数学模型, 考虑系统的非完整约束特性, 提出太阳帆板展开过程的最优控制算法. 通过数值仿真, 表明该方法对太阳帆板展开姿态控制的有效性. 相似文献
52.
A.V. Oinats K.G. RatovskyG.V. Kotovich 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2008
We present an investigation of the influence of the 27-day solar flux variations, caused by solar rotation, on the ionosphere parameters such as the F2 layer critical frequency (foF2) and the total electron content (TEC). Our observational data were obtained with the Irkutsk Digisonde (DPS-4) located at 52.3 North and 104.3 East during the period from 2003 to 2005. In addition, we use TEC data from the Global Ionosphere Maps (GIM) based on Global Positioning System (GPS) satellites. The solar radiation flux at a wavelength of 10.7 cm (F10.7 index) is used as an index characterizing the solar activity level. A good correlation between observed ionosphere parameters and solar activity variations is found especially in autumn-to-winter season. We estimate the impact of the 27-day solar flux variations on the day-to-day variability and determine the time delay of the ionosphere response. 相似文献
53.
本文例举观测实例说明,在宁静太阳风中或重现太阳风的低速流区,有可能形成行星际亚阿尔文波速流。这种流出现在阿尔文波速异常增强区,并与特定的磁场位形相联系。 相似文献
54.
为了改善光学遥感卫星的成像质量,提升卫星操控的灵活性,基于遥感成像理论,提出了依据太阳高度角的卫星在轨成像参数自主调整方法。文中首先讨论了影响卫星遥感成像质量的因素,分析了入瞳辐亮度随太阳高度角的变化规律及在不同侧摆角时,一个轨道周期内相机积分时间的变化范围,并据此建立了太阳高度角、侧摆角与积分级数、增益的对应关系。然后分析了太阳高度角和侧摆角的最佳分挡策略,最终得到了可用于卫星在轨成像参数自主调整的二维查找表,以实现卫星在轨成像参数自主调整。利用该方法可提升图像的辐射质量,极大减少了地面上注的数据量。 相似文献
55.
高空气球标定的太阳能电池是可被用于地面太阳模拟器和太阳光光强检测的标准电池。首先,给出了由飞行气球搭载的高空太阳能电池标定所使用的太阳跟踪控制系统设计方法,包括基于STM32的太阳跟踪控制系统硬件设计方案、混合自动追踪控制策略、软件开发与实现方法、高空跟踪控制技术问题解决方案以及高空标定试验等。同时,解决了高空气球电池标定用太阳跟踪控制系统在极端环境下高可靠性、连续追踪和防抖动等关键技术问题。试验结果为气球飞行高度32km,平飘时间超过2h,太阳跟踪偏差小于1°。经初步分析,高空太阳跟踪控制系统标定测试结果合理可靠,工作性能稳定,为中国高空气球太阳能电池AM0标定用太阳跟踪控制系统的研究提供了新思路。 相似文献
56.
We review work on diffusion coefficients of energetic particles with an attempt to extract implications on their behaviour at high latitudes. In the ecliptic plane results from solar energetic particle propagation between the Sun and about 5 AU can be described by an effective radial mean free path
r
which is approximately constant as a function of distancer. When particle propagation in three dimensions in the heliosphere is considered it is not sufficient to consider
r
only. Jovian electrons can be used as probes to determine the parameters of three-dimensional diffusion. In the polar regions diffusion is dominated by its parallel component. Some predictions how should vary with latitude are discussed. For different choices of this variation we present expectations for intensity-time profiles of solar particle events during the Ulysses polar passages. 相似文献
57.
Recent data and theory for type II solar radio bursts are reviewed, focusing on a recent analytic quantitative theory for
interplanetary type II bursts. The theory addresses electron reflection and acceleration at the type II shock, formation of
electron beams in the foreshock, and generation of Langmuir waves and the type II radiation there. The theory's predictions
as functions of the shock and plasma parameters are summarized and discussed in terms of space weather events. The theory
is consistent with available data, has explanations for radio-loud/quiet coronal mass ejections (CMEs) and why type IIs are
bursty, and can account for empirical correlations between type IIs, CMEs, and interplanetary disturbances.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
58.
Kamide Y. Kihn E.A. Ridley A.J. Cliver E.W. Kadowaki Y. 《Space Science Reviews》2003,107(1-2):307-316
We report the recent progress in our joint program of real-time mapping of ionospheric electric fields and currents and field-aligned
currents through the Geospace Environment Data Analysis System (GEDAS) at the Solar-Terrestrial Environment Laboratory and
similar computer systems in the world. Data from individual ground magnetometers as well as from the solar wind are collected
by these systems and are used as input for the KRM and AMIE magnetogram-inversion algorithms, which calculate the two-dimensional
distribution of the ionospheric parameters. One of the goals of this program is to specify the solar-terrestrial environment
in terms of ionospheric processes, providing the scientific community with more than what geomagnetic activity indices and
statistical models provide.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
59.
Alexeev Igor I. Belenkaya Elena S. Bobrovnikov Sergey Yu. Kalegaev Vladimir V. 《Space Science Reviews》2003,107(1-2):7-26
A magnetohydrodynamic model of the solar wind flow is constructed using a kinematic approach. It is shown that a phenomenological
conductivity of the solar wind plasma plays a key role in the forming of the interplanetary magnetic field (IMF) component
normal to the ecliptic plane. This component is mostly important for the magnetospheric dynamics which is controlled by the
solar wind electric field. A simple analytical solution for the problem of the solar wind flow past the magnetosphere is presented.
In this approach the magnetopause and the Earth's bow shock are approximated by the paraboloids of revolution. Superposition
of the effects of the bulk solar wind plasma motion and the magnetic field diffusion results in an incomplete screening of
the IMF by the magnetopause. It is shown that the normal to the magnetopause component of the solar wind magnetic field and
the tangential component of the electric field penetrated into the magnetosphere are determined by the quarter square of the
magnetic Reynolds number. In final, a dynamic model of the magnetospheric magnetic field is constructed. This model can describe
the magnetosphere in the course of the severe magnetic storm. The conditions under which the magnetospheric magnetic flux
structure is unstable and can drive the magnetospheric substorm are discussed. The model calculations are compared with the
observational data for September 24–26, 1998 magnetic storm (Dst
min=−205 nT) and substorm occurred at 02:30 UT on January 10, 1997.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
60.