GNSS无线电掩星大气探测混合星座设计

针对目前GNSS无线电掩星大气探测卫星星座参数依赖大量仿真计算进行统计选取的研究现状,通过将探测卫星星下点与大气测点间地心角距作为观测半径提出了一种虚拟“星—地”遥感假设,给出了一种崭新的掩星测点预估方法,具有计算速度快的特点.基于该方法推导了探测星座参数与大气探测覆盖性之间的极值相关特性,建立了GNSS无线电掩星大气探测卫星星座设计准则,并以GPS和BD为兼容性观测信源完成了GNSS掩星大气探测混合卫星星座设计.通过仿真试验,验证了设计方法的快速性和可行性,GPS+BD掩星大气探测混合星座每日可实现掩星探测量为COSMIC星座的3倍以上,12h内掩星测点全球分布均匀度提升12％.     

联合地基GNSS及空基GNSS掩星探测水汽三维分布

研究了联合地基GNSS和空基GNSS掩星观测的大气水汽探测方法。首先,利用COSMIC(气象、电离层、气候星座观测系统)和GRACE(重力恢复与气候实验)无线电掩星产品对对流层层析成像的几个关键技术进行了优化,标定了对流层干延迟模型,建立了新的大气加权平均温度模型,提出了一种新方法用于确定水汽层层顶(即对流层层析模型的顶部边界)。选择香港地区12个连续GNSS气象监测站2017年6月份的数据反演计算了水汽的三维分布,以探空测站的水汽密度为真值,统计层析反演结果与真值之间的偏差为:偏差平均值优于1.36g/m~3,RMS值优于1.70g/m~3。     

基于微波辐射测量的电波折射修正技术

针对电波折射修正精度直接影响无线电系统的探测和定位精度这一问题,提出了利用微波辐射计反演大气折射率剖面进行电波折射修正的解决方法,并引入RBF（Radial Basis Function,径向基）神经网络算法反演大气折射率.在青岛市气象局架设MP-3000A型多通道微波辐射计,开展了长达1个月的与探空数据的联合观测比对实验,对输出的大气折射率剖面进行了详细的分析.实验结果表明：RBF神经网络算法与MP-3000A自带的神经网络算法相比,反演大气折射率剖面的精度提高了30％以上,同时,电波折射修正的精度也得以提高.因此,利用微波辐射计反演大气折射率剖面进行电波折射修正方法可行.     

基于星载加速度计反演载人航天轨道大气密度

热层大气密度直接影响低轨道航天器的精密定轨,热层大气密度模型的误差是影响载人航天定轨精度的关键因素。选取400km为载人航天轨道的代表高度,利用CHAMP卫星数据修正热层大气密度模型,进而反演得到2002年的热层大气密度,统计其中长期变化特征,并分析大气密度与太阳活动和地磁活动的关系,得出热层大气密度与两种指数的总体变化趋势一致的结论,且地磁活动与大气密度的相关性更好。同时将大气密度的反演值与神舟三号飞船的实测密度值进行对比,结果显示二者有较好的一致性,其平均残差和均方根误差分别为0．03和0．24,并且地磁平静期的误差明显小于磁暴期。结果表明,利用星载加速度计数据反演载人航天轨道大气密度是一种有效的方法。     

高轨目标掩星成像相位恢复技术研究

高轨目标掩星成像通过观测高轨卫星对恒星的遮掩过程,实现对高轨目标的成像.该方法采用望远镜线性阵列观测高轨目标遮掩恒星过程中恒星亮度变换,获得高轨目标在地面的投影,通过相位恢复方法可计算得到卫星轮廓图样,具有成像分辨力高,设备制造难度小等优点,在高轨目标成像领域具有较好应用前景.本文分析利用掩星成像方法对高轨目标成像的可行性,重点对掩星成像过程的相位恢复方法进行改进,根据掩星成像特点对输入输出算法进行优化,仿真结果表明：改进后的相位恢复方法可显著提高图像恢复质量和掩星成像方法的空间分辨力.     

可实时重构的国际C站卫星模拟器

我国自行研制的国际标准C频段统一测控系统,配置了功能齐全的卫星模拟器,但其一星一模拟器的方式已不能适应当前多星管理和未来星座管理的需要。本文旨在探讨利用现有的微波宽带器件技术和软件无线电技术,用一套硬件系统,根据需要实时重构成所需卫星的模拟器,达到多星共用一套模拟器,实现小型化、实时性的目的。     

地基单站GPS探测大气折射环境

基于地基单站双频GPS接收机,提出了实时遥感探测大气折射环境（包括对流层折射率剖面与电离层电子密度剖面）的方法,并经过实验验证可行。在对流层方面,改进精密单点定位技术使得对流层低仰角斜延迟可以实时解算,然后利用相关向量机方法反演得到对流层折射率剖面;在电离层方面,采用Kalman滤波技术消除硬件延迟得到电离层TEC,基于IRI模型,利用遗传算法反演得到电离层电子密度剖面。此研究为大气折射环境的实时、高效、低成本探测提供了一种新手段。     

用全球定位系统对近地卫星进行高精度定轨

业已证明近地卫星在地球动力学和海洋学研究方面是非常有用的。但是,一项重要限制是卫星轨道状态的确定精度。一般通过处理由地面跟踪网所获得的无线电跟踪数据进行卫星定轨。使用这种地面无线电技术,目前所能达到的定轨精度为米级。对于地球动力学应用和完成海洋学的研究,必须将大地水准面测定到1m以下。本文研究一种应用GPS的定轨技术,采用新的测量方法和数据处理方法可改善定轨精度。我们利用干涉测量的方法来完成用户卫星的高精度定位。巧妙布置少量地面站,使任何一对地面站和用户星总能看见4颗以上的GPS卫星组成的星座。接着本文介绍了使用无线电干涉测量值定轨的误差分析结果,结果表明通过事后数据处理,用这种技术,卫星位置精度可达到所需要的分米级。给出的结果还表明无线电干涉测量对更精确的地球卫星轨道确定也是很有价值的。     

月球探测器天文测角/单程无线电时间差分测距/差分测速导航方法

月球探测器高精度导航技术是确保月球探测任务顺利实施的关键技术之一。当前,大多数月球探测器都是利用地面无线电进行导航和控制,但存在可测控弧段短、易受干扰等局限性,且对于月球背面探测,存在无法直接测控的不足。针对上述问题,提出了一种新的基于天文测角/单程无线电差分测距/差分测速的月球探测器组合导航方法。该方法使用了天文星光角距、探测器接收到的来自地面站或中继星的单程无线电时间差分测距和时间差分多普勒测速3种量测信息,可有效抑制星上时钟和频谱仪的时间和频率测量误差。收敛后的平均位置和速度估计误差分别为902.7 m和0.12 m/s,最大的位置和速度估计误差分别为1 548.2 m和0.24 m/s。仿真分析结果表明该方法具有较高自主导航精度。     

双通道微波辐射计大气折射率剖面反演的神经网络算法

基于地基双通道微波辐射计（23．8GHz和31．65GHz）所测天顶方向的亮温测量数据和地面气象参数，给出了一种利用微波辐射测量反演大气折射率剖面的神经网络算法。利用青岛地区历史探空数据仿真的大气辐射亮温对神经网络进行了训练，回归得到了三段折射率剖面模型，并对利用实测亮温反演的大气折射率剖面与探空实测折射率剖面和模式剖面进行了比较分析，分析结果表明利用微波辐射计反演的折射率剖面与实测剖面间有很好的一致性，较三段折射率剖面模式具有更好的反演精度。     

Lower and Upper Ionosphere of Mars

The ionosphere of Mars has been explored mostly with the radio occultation experiment onboard Mariners 6, 7, 9; Mars 2, 3, 4, 6; Viking 1, 2, and more recently on Mars Global Surveyor (MGS) and Mars Express (MEX). In addition to the radio occultation experiment, MEX also carried Mars Advanced Radar for the Subsurface and Ionosphere Sounding (MARSIS) experiment which provided electron density profiles well above the main ionospheric peak. The atmosphere of Mars was measured directly by the neutral mass spectrometer onboard Viking 1 and 2 Landers. Later, an accelerometer and radio occultation experiment on MGS provided large data sets of atmospheric density at various locations in the upper and lower atmospheres of Mars, respectively. In this paper we review results of these upper and lower atmospheric/ionospheric measurements. Results of these measurements have been compared with theoretical models by several workers; therefore, we also review various atmospheric and ionospheric models of Mars.     

The New Horizons Radio Science Experiment (REX)

The New Horizons (NH) Radio Science Experiment, REX, is designed to determine the atmospheric state at the surface of Pluto and in the lowest few scale heights. Expected absolute accuracies in n, p, and T at the surface are 4?10¹⁹ m^?3, 0.1 Pa, and 3 K, respectively, obtained by radio occultation of a 4.2 cm-λ signal transmitted from Earth at 10–30 kW and received at the NH spacecraft. The threshold for ionospheric observations is roughly 2?10⁹ e^??m^?3. Radio occultation experiments are planned for both Pluto and Charon, but the level of accuracy for the neutral gas is expected to be useful at Pluto only. REX will also measure the nightside 4.2 cm-λ thermal emission from Pluto and Charon during the time NH is occulted. At Pluto, the thermal scan provides about five half-beams across the disk; at Charon, only disk integrated values can be obtained. A combination of two-way tracking and occultation signals will determine the Pluto system mass to about 0.01 percent, and improve the Pluto–Charon mass ratio. REX flight equipment augments the NH radio transceiver used for spacecraft communications and tracking. Implementation of REX required realization of a new CIC-SCIC signal processing algorithm; the REX hardware implementation requires 1.6 W, and has mass of 160 g in 520 cm³. Commissioning tests conducted after NH launch demonstrate that the REX system is operating as expected.     

Radio science investigations with Voyager

The planned radio science investigations during the Voyager missions to the outer planets involve: (1) the use of the radio links to and from the spacecraft for occultation measurements of planetary and satellite atmospheres and ionospheres, the rings of Saturn, the solar corona, and the general-relativistic time delay for radiowave propagation through the Sun's gravity field; (2) radio link measurements of true or apparent spacecraft motion caused by the gravity fields of the planets, the masses of their larger satellites, and characteristics of the interplanetary medium; and (3) related measurements which could provide results in other areas, including the possible detection of long-wavelength gravitational radiation propagating through the Solar System. The measurements will be used to study: atmospheric and ionospheric structure, constituents, and dynamics; the sizes, radial distribution, total mass, and other characteristics of the particles in the rings of Saturn; interior models for the major planets and the mean density and bulk composition of a number of their satellites; the plasma density and dynamics of the solar corona and interplanetary medium; and certain fundamental questions involving gravitation and relativity. The instrumentation for these experiments is the same ground-based and spacecraft radio systems as will be used for tracking and communicating with the Voyager spacecraft, although several important features of these systems have been provided primarily for the radio science investigations.     

大气密度模型用于近地卫星定轨预报的比较

大气阻力是低轨卫星主要的摄动力,与高层大气密度的变化密切相关。由于目前对高层大气密度变化的机制尚未完全掌握,所使用的各种大气密度模型多属于半经验公式。在这些模型中并没有一种在任何情况下都是最好的,因此,对于特定轨道选择合适的大气密度模型对提高定轨预报的精度是非常重要的。通过对资源2号卫星实测GPS数据的分析计算,比较了常用的8种大气密度模型的定轨预报精度,探讨了预报24h应采用的定轨数据长度和大气密度模型。     

磁暴下的LEO卫星精密轨道确定

对低轨卫星（LEO）,大气阻尼摄动是主要的定轨误差源.尤其在发生磁暴时,求解一个大气阻尼因子的定轨方法已不能充分吸收大气密度计算不准所造成的定轨误差,因而在标校统一S波段（USB）的测量系统差和随机差时往往计算失真.本文提出了一种求解折线型Cd因子的新方法,克服了动力学模型不准所带来的定轨误差,通过与独立的GPS数据比较,定轨精度有明显提高,同时给出的测量系统差和随机差更加真实可信.     

Fuel-optimal trajectories of aeroassisted orbital transfer withplane change

The fuel-optimal control problem arising in noncoplanar orbital transfer employing aeroassist technology is addressed. The mission involves the transfer from high Earth orbit to low Earth orbit with plane change. The complete maneuver consists of a deorbit impulse to inject a vehicle from a circular orbit to an elliptic orbit for atmospheric entry, a boost impulse at the exit from the atmosphere for the vehicle to attain a desired orbital altitude, and a reorbit impulse to circularize the path of the vehicle. In order to minimize the total fuel consumption, a performance index is chosen as the sum of the deorbit, boost, and reorbit impulses. The application of optimization principles leads to a nonlinear, two-point, boundary value problem, which is solved by a multiple shooting method     

Galileo radio science investigations

The radio science investigations planned for Galileo's 6-year flight to and 2-year orbit of Jupiter use as their instrument the dual-frequency radio system on the spacecraft operating in conjunction with various US and German tracking stations on Earth. The planned radio propagation experiments are based on measurements of absolute and differential propagation time delay, differential phase delay, Doppler shift, signal strength, and polarization. These measurements will be used to study: the atmospheric and ionospheric structure, constituents, and dynamics of Jupiter; the magnetic field of Jupiter; the diameter of Io, its ionospheric structure, and the distribution of plasma in the Io torus; the diameters of the other Galilean satellites, certain properties of their surfaces, and possibly their atmospheres and ionospheres; and the plasma dynamics and magnetic field of the solar corona. The spacecraft system used for these investigations is based on Voyager heritage but with several important additions and modifications that provide linear rather than circular polarization on the S-band downlink signal, the capability to receive X-band uplink signals, and a differential downlink ranging mode. Collaboration between the investigators and the space-craft communications engineers has resulted in the first highly-stable, dual-frequency, spacecraft radio system suitable for simultaneous measurements of all the parameters normally attributed to radio waves.