共查询到19条相似文献，搜索用时 125 毫秒
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我国低轨道卫星定轨精度分析 总被引：7，自引：0，他引：7
朱文耀 《中国科学院上海天文台年刊》1998,(19):58-67
针对高度在250－350km的三颗低轨道卫星,根据我国现有的卫星跟踪网和跟踪技术（雷达测距和多普勒测速）等观测条件,利用模拟方法估计和分析了各种误差源对定轨精度的影响,并对能达到的定轨精度进行了恰如其分的估计。 相似文献
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在全球导航卫星系统中,定位精度是一个重要的性能指标。准确的定位误差模型有利于理解系统的工作模式,同时也为进一步提高系统性能提供指导。当卫星的测距误差满足相互独立和方差均一的条件时,定位误差等于测距误差标准差与几何精度因子的乘积。然而在实际应用中,由于不同卫星信号的传播路径不同,测距误差的统计特征难以相同,尤其当卫星信号受到多径干扰与电离层闪烁影响时,不同卫星间的测距误差有显著的差异。介绍了一种利用奇异值分解方法建立的非均一测距误差的定位误差理论模型,利用北京站与香港站的实测数据,对受到多径效应与电离层闪烁影响的定位误差进行分析。结果表明,其统计特性与非均一方差的定位误差模型给出的结果一致,验证了模型的正确性和有效性。 相似文献
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Yang Kejun 《时间频率学报》1995,(1)
本文分析了利用中国科学院陕西天文台的流星雷达进行人为空间碎片监测的可能性．详细计算了到达接收机的回波的信噪比Ｓ／Ｎ依赖于目标散射横截面。和高度距离Ｒ的关系。理论计算表明，利用陕西天文台的流星雷达完全有可能监测在２００ｋｍ至１２００ｋｍ的高度范围内，半径大于０．５ｍ的人为空间碎片． 相似文献
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用陕西天文台流星雷达监测人为空间碎片可能性的分析 总被引：1，自引：0，他引：1
本文分析了利用中国科学院陕西天文台的流星雷达进行人为间空碎片监测的可能性。详细计算了到达接收机的回波的信噪比Ｓ／Ｎ依赖于目标散射截面σ和高度距离Ｒ的关系。理论计算表明，利用陕西天文台的流星雷达完全有可能监测在２００ｋｍ至１２００ｋｍ的高度范围内，半径大于０。５ｍ的人为空间碎片。 相似文献
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环月飞行器精密定轨的模拟仿真 总被引：11，自引：2，他引：11
以中国正在实施的探月计划“嫦娥1号”工程为背景，分析了在中国联合S波段(USB)测控网和甚长基线射电干涉(VLBI)跟踪网的现有空间分布、观测精度水平下的环月飞行器精密定轨．采用的方法是模拟仿真计算，即首先模拟观测数据，然后在计入各误差源的影响后进行求解，并对解算结果进行比较．模拟仿真的工具是美国宇航局哥达德飞行中心的空间数据分析软件系统GEODYN．环月飞行的主要误差源是月球重力场，为此首先讨论了目前精度最高的月球重力场模型JGL165P1的(形式)误差．在模拟了测距、测速以及VLBI的时延、时延率数据后，计入月球重力场的误差进行精密轨道确定．定轨时采用了减缩动力学(reduced dynamic)方法，即选用合适的经验加速度参数吸收重力场误差对定轨的影响．结果表明对于一个不将月球重力场作为主要科学目标的探月计划(如“嫦娥1号”)，减缩动力学方法是一个简单、有效地提高环月飞行器定轨精度的方法． 相似文献
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提出一种简易的卫星电视接时系统，它搭载现已插入时频信息的卫星电视系统，增加一套对卫星的测距设备，将测距值插入电视信号中，就使卫星电视系统在中国境内具有精度达十几μｓ的授时功能． 相似文献
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V. V. Sidorov S. A. Kalabanov D. V. Lyubimov A. F. Nasyrov A. D. Sidorova I. V. Filin 《Solar System Research》2008,42(3):194-208
The results of an analysis of the orbital structure of the meteor complex accessible for radar observations at northern midlatitudes are reported. Experimentally, the study is based on the long-term monitoring of the influx of meteor matter into the Earth’s atmosphere performed with the meteor radar of Kazan State University starting from 1986. The study uses a discrete quasi-tomographic method to measure the radiants and velocities of meteor showers based on goniometric data of the meteor radar and diffraction measurements of meteor velocities. The discretization of the detection environment—in particular, in terms of velocity—is shown to result in no substantial loss of measurement accuracy. The error of the measured velocity of the shower does not exceed 1.5 km/s for a standard deviation of a single velocity measurement equal to 3 km/s. Microshower representation is used with microshowers either representing the correlated part of the sporadic complex or being partial streams of major and minor showers, or fragments of the dust environment of minor bodies passing by Earth or falling onto it. The data of measurements made over the entire annual cycle are used to construct combined maps of the distribution of the observed 2263 microshowers (a total of 22 604 orbits) by their inclination, aphelion distance, and longitudes of the ascending nodes of their orbits. The observing conditions are shown to have a significant effect on the parameters of the distribution of aphelion distances for different months, and the corresponding distributions for prograde and retrograde orbits are shown to differ fundamentally. A specific feature of such distribution maps is that they allow uniform representation of both meteor showers and irregularities of the sporadic complex. 相似文献
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J.D. Mathews M.P. Sulzer C.A. Tepley R. Bernard J.L. Fellous M. Glass M. Massebeuf S. Ganguly R.M. Harper R.A. Behnke J.C.G. Walker 《Planetary and Space Science》1981,29(3):341-348
The results of simultaneous meteor and Thomson scatter radar wind measurements in the 65–105 km altitude region are presented. The two radars are located in Puerto Rico where the 430-MHz Thomson scatter radar at Arecibo Observatory is employed along with the French (CNET) portable meteor radar which is at a 40-km distance. The two sets of wind measurements compare quite favorably during periods of coincident observation. The meteor radar yields continuous results while the Thomson scatter radar is usable only during daylight hours. The Thomson scatter results, on the other hand, extend down to 65 km altitude and are available with better height and time resolutions than the meteor radar results. The two measurement techniques are therefore complementary. 相似文献
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The meteor radar response function is an important tool for analyzing meteor backscatter observed by radar systems. We extend previous work on the development of the response function to include a non-uniform meteor ionization profile, provided by meteor ablation theory, in contrast to what has been assumed in the past. This has the advantage that the height distribution of meteors expected to be observed by a radar meteor system may be accurately modeled. Such modeling leads to meteor height distributions that have implications for the composition of those meteoroids ablating at high altitudes which may be observed by “non-traditional” meteor radars operating at MF/HF. The response function is then employed to investigate meteor backscatter observed by narrow beam MST radars which in recent years have been used increasingly to observe meteors. 相似文献
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The height distributions, velocity distributions and flux measurements of underdense echoes determined from meteor radar observations are significantly affected by the attenuation associated with the initial radius of meteor trains. Dual-frequency radar observations of a very large set of sporadic radar meteors at 29 and 38 MHz yield estimates of the initial train radius and its dependence on height and meteoroid speed as determined by the time-delay method. We provide empirical formulae that can be used to correct meteoroid fluxes for the effect of initial train radius at other radio frequencies. 相似文献
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We tested four criteria used for discrimination between asteroidal and cometary type of orbits: Whipple criterion K, Kresak
criterion Pe, Tisserand invariant T and aphelion distance Q. To estimate their reliability, all criteria were applied to classify
the 2225 orbits of NEAs and 582 orbits of comets, for several epochs spanning the time interval of 40 thousands years. The
Q-criterion produced the smallest number of exceptions and has shown the best stability. The biggest number of exceptions
and the biggest variations are obtained for the K-criterion. We applied the Q-criterion to classify meteor orbits from the
IAU Meteor Data Center and the video meteor orbits available on the Web sites. Among the sporadic radar orbits, as well as
among the mean orbits of meteor streams a strong preponderance of asteroid-type orbits was observed. In case of the photographic
and video meteors a weak preponderance of cometary and asteroidal orbits was found, respectively. 相似文献
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We present a method to calculate the radiation pressure force to gravity ratio on meteoroids from their atmospheric flight. Radiation pressure corrections to meteor orbits are negligible for fireballs; of the order of or less than the measurement errors (≈ 1%) for photographic meteors; of the order of and in some cases substantially larger than the measurement errors (≈ 10%) for radar meteors. 相似文献
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Lars P. Dyrud Kelly Denney Julio Urbina Diego Janches Erhan Kudeki Steve Franke 《Earth, Moon, and Planets》2004,95(1-4):89-100
In this paper, we use radar observations from a 50 MHz radar stationed near Salinas, Puerto Rico, to study the variability
of specular as well as non-specular meteor trails in the E-region ionosphere. The observations were made from 18:00 to 08:00 h
AST over various days in 1998 and 1999 during the Coqui II Campaign [Urbina et al., 2000, Geophys. Rev. Lett. 27, 2853–2856]. The radar system had two sub-arrays, both produced beams pointed to the north in the magnetic meridian plane,
perpendicular to the magnetic field, at an elevation angle of approximately 41 degrees.
The Coqui II radar is sensitive to at least two types of echoes from meteor trails: (1) Specular reflections from trails oriented
perpendicular to the radar beam, and (2) scattering, or, non-specular reflections, from trails deposited with arbitrary orientations.
We examine and compare the diurnal and seasonal variability of echoes from specular and non-specular returns observed with
the Coqui II radar. We also compare these results with meteor head echo observations made with the Arecibo 430 MHz radar.
We use common region observations of these three types of meteor echoes to show that the diurnal and seasonal variability
of specular trails, non-specular trails, and head echoes are not equivalent. The implications of these results on global meteor
mass flux estimates obtained from specular meteor observations remains to be examined. 相似文献
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Lars Dyrud Derek Wilson Steiner Boerve Jan Trulsen Hans Pecseli Sigrid Close Chen Chen Yoonjae Lee 《Earth, Moon, and Planets》2008,102(1-4):383-394
Recently, meteor head echo detections from high powered large aperture radars (HPLA) have brought new measurements to bear
on the study of sporadic interplanetary meteors. These same observations have demonstrated an ability to observe smaller meteoroids
without some of the geometrical restrictions of specular radar techniques. Yet incorporating data from various radar reflection
types and from different radars into a single consistent model has proven challenging. We believe this arises due to poorly
understood radio scattering characteristics of the meteor plasma, especially in light of recent work showing that plasma turbulence
and instability greatly influences meteor trail properties at every stage of evolution. In order to overcome some of the unknown
relationships between meteoroid characteristics (such as mass and velocity) and the resulting head echo radar cross-sections
(RCS), we present our results on meteor plasma simulations of head echo plasmas using particle in cell (PIC) ions, which show
that electric fields strongly influence early stage meteor plasma evolution, by accelerating ions away from the meteoroid
body at speeds as large as several kilometers per second. We also present the results of finite difference time domain electromagnetic
simulations (FDTD), which can calculate the radar cross-section of the simulated meteor plasma electron distributions. These
simulations have shown that the radar cross-section depends in a complex manner on a number of parameters. In this paper we
demonstrate that for a given head echo plasma the RCS as a function of radar frequency peaks at sqrt (2*peak plasma frequency)
and then decays linearly on a dB scale with increasing radar frequency. We also demonstrate that for a fixed radar frequency,
the RCS increases linearly on a dB scale with increasing head echo plasma frequency. These simulations and resulting characterization
of the head echo radar cross-section will both help relate HPLA radar observations to meteoroid properties and aid in determining
a particular radar facility’s ability to observe various meteoroid populations. 相似文献
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We discuss a new method for measuring the coordinates of meteor shower radiants from meteor radar data. The method uses a high accuracy of radar goniometer measurements of one of the angular coordinates for meteor radiants and collective properties of incident meteor showers. It is based on a computer technology of searching for the coordinates of radiants using the intersections of meteor position lines on the celestial sphere and filtering nonrandom combinations of these intersections. The method allows the following: to detect meteor showers with a rate of more than 5 per day of observations and to separate meteor groups from different meteor showers with different radiants and velocities. The method makes it possible to increase the angular resolution from 10° × 10° achieved with a quasi-tomographic technique to 2° × 2°, with a prospect of a further increase in the accuracy through the individual reduction of separated meteor groups. We use the reduction of one-day-long observations during maximum activity of the Geminids meteor shower in 1993 to illustrate the potentialities of the method. We show an example of detecting a weak meteor shower that was active during December 1993. 相似文献