云台40m射电望远镜的指向误差校正

首先综述了射电望远镜指向误差校正的原理并对软件校准的两种方法进行了比较。其次阐述了利用软件校准的方法对云南天文台40m射电望远镜进行指向校正的过程,并给出其指向校正结果。结果是经过指向校正后该射电望远镜的指向精度达到观测要求。     

轨道不平度对天线指向的影响分析与修正

基于天线轨道不平度对望远镜指向的影响机理,测量并分析采用整体焊接轨道技术后的乌鲁木齐南山26 m射电望远镜(NanShan Radio Telescope,NSRT)天线轨道误差的分布情况及对指向的影响,从而对指向模型进行修正.采用移动最小二乘法(Moving Least-Squares,MLS)将测得的天线轨道高度差拟合成一个闭合的轨道高度分布曲线,确定因轨道不平度影响的天线方位轴偏差,对比实测天线座架变形的方位轴偏差,发现二者具有较强的相关性.考虑到天线座架重力变形的偏差包含南北向和东西向偏差,建立新的指向偏差模型进行校正.最后通过对已知校准射电源进行扫描测量,将指向偏差数据进行拟合.结果表明:新建的指向修正模型能够抑制已知指向模型偏差中的正弦分量,从而说明所建模型很好地反映了天线的指向偏差并对偏差具有一定修正作用.     

射电天线指向改正模型中轴系误差的完全表达式

为了提高射电天线的目标跟踪精度,采用直接法推导了射电天线轴系误差对指向的影响,并给出轴系误差指向改正模型的完全表达式,明确了指向改正模型中各轴系参数的定义,传统分项以及球谐函数所推导的轴系误差项为该模型的简化形式.基于此,评估得出基本参数改正模型中,因忽略轴系误差高次谐项而引起的指向精度损失可能达到1′′量级,具体需结合轴系误差大小而定;同时明确了基本参数改正模型(如22项指向模型)中与轴系误差有关的部分高次谐项系数的物理意义.为高精度轴系误差指向改正模型的建立提供了理论依据.     

佘山25米天线导轨问题对指向误差影响的研究

本根据25米射电望远镜方位导轨水平度的检测数据，分析了天线在不同位置时指向误差的情况及其原因，为进一步提高天线指向精度提供了理论依据和实测数据。     

主反射面变形引起的天线指向误差修正方法

射电天线指向精度通常要求小于主波束宽度的1/10, 对于短厘米波段或毫米波段的大口径反射面天线, 指向精度要求高达几个角秒, 对于天线性能目标的实现是个巨大的挑战, 因此对于大口径高频段的反射面天线来说指向问题成为天线性能实现的重要关注焦点. 在众多影响天线指向精度的结构子系统因素中, 对主反射面变形因素的研究很少. 文章结合天线的结构特点建立了反射面空间坐标系统, 并基于变形后主面点的空间坐标值, 提出了3自由度下的非线性最小二乘吻合的方法去精准预测天线指向. 最后利用空间几何关系严格推导出了服务于天线指向误差修正的俯仰和方位的精确调整量, 从而构建了主面变形同指向误差之间的间接关系, 这对大型射电天线指向精度的提升具有一定的指导意义.     

地平式望远镜轴系误差对指向精度和跟踪精度的影响

采用球面几何的方法推导轴系位置误差对地平式望远镜指向、跟踪精度影响的计算模型.介绍2米级地平式望远镜轴系误差检测及数据处理方法.通过对目标星体指向、跟踪仿真,得到轴系位置误差对指向、跟踪精度影响规律,为轴系精度及轴系位置要求提供理论依据,并为后续控制修正提供参考模型.     

南极5 m太赫兹望远镜指向与调焦校准精度分析

指向校准与副面调焦是天线测量的重要组成部分,对射电望远镜实际的观测性能有重要影响.根据南极5 m太赫兹望远镜(DATE5)指向精度和离焦增益损失的指标要求,计算得到了指向校准与副面调焦观测过程中对信噪比的要求,并以此为依据选取了若干可行的候选校准源,包括太阳系行星和超致密电离氢区.分析了大气吸收和校准源角直径对测量精度的影响.仿真分析结果表明:望远镜在南极工作时,这些校准源在一定的高度角范围内可以提供足够强的流量密度,用来验证预先建立的太赫兹和光学望远镜两光轴指向偏差模型以及副面调焦模型.     

25米天线电性能参数测试

本叙述了上海天台25米射电望远镜天线电性能参数，即天线效率、天线噪声温度（天线指向偏离观测源时的天线等效噪声温度）及天线主瓣半功率宽度等的测量原理、方法和结果。     

大型天线轮轨接触研究综述

大型天线的发展对指向跟踪精度提出更高的要求。当大型射电天线方位转动部分采用轮轨式结构时,轮轨精度对指向误差的影响、轮轨的磨损成了亟待解决的问题。首先论述了轮轨式天线座的优缺点．回顾了国内外现有典型的射电天线在轮轨结构系统方面以及指向误差修正方法的研究现状：并借鉴了轨道交通系统与轮轨式起重机系统的研究成果,介绍了轮轨接触理论自创立以来形成的经典理论及其存在的局限性．最后总结了轮轨式天线座轮轨接触研究存在的问题及研究方向。     

用天鹅A校准密云米波综合孔径系统

本文从理论上分析了使用已知射电源校准干涉仪基线与相位的方法。使用强源天鹅A(以下简称Cyg A)校准了密云系统的仪器相位并对干涉仪的基线误差给出估计。在校准工作中,利用了CygA坐标所带来的方便,同时成功地解决了计算机上相位识别的问题。     

On the theory of the oblateness of the Sun

In this paper we first emphasize why it is important to know the successive zonal harmonics of the Sun's figure with high accuracy: mainly fundamental astrometry, helioseismology, planetary motions and relativistic effects. Then we briefly comment why the Sun appears oblate, going back to primitive definitions in order to underline some discrepancies in theories and to emphasize again the relevant hypotheses. We propose a new theoretical approach entirely based on an expansion in terms of Legendre's functions, including the differential rotation of the Sun at the surface. This permits linking the two first spherical harmonic coefficients (J ₂ and J ₄) with the geometric parameters that can be measured on the Sun (equatorial and polar radii). We emphasize the difficulties in inferring gravitational oblateness from visual measurements of the geometric oblateness, and more generally a dynamical flattening. Results are given for different observed rotational laws. It is shown that the surface oblateness is surely upper bounded by 11 milliarcsecond. As a consequence of the observed surface and sub-surface differential rotation laws, we deduce a measure of the two first gravitational harmonics, the quadrupole and the octopole moment of the Sun: J ₂=−(6.13±2.52)×10⁻⁷ if all observed data are taken into account, and respectively, J ₂=−(6.84±3.75)×10⁻⁷ if only sunspot data are considered, and J ₂=−(3.49±1.86)×10⁻⁷ in the case of helioseismic data alone. The value deduced from all available data for the octopole is: J ₄=(2.8±2.1)×10⁻¹². These values are compared to some others found in the literature. Supplementary material to this paper is available in electronic form at http://dx.doi.org/10.1023/A:1005238718479     

Accounting for the viscosity of the fluid core in the problem of the physical libration of the moon

A two-component theoretical model of the physical libration of the Moon in longitude is constructed with account taken of the viscosity of the core. In the new version, a hydrodynamic problem of motion of a fluid filling a solid rotating shell is solved. It is found that surfaces of equal angular velocity are spherical, and a velocity field of the fluid core of the Moon is described by elementary functions. A distribution of the internal pressure in the core is found. An angular momentum exchange between the fluid core and solid mantle is described by a third-order differential equation with a right-hand side. The roots of a characteristic equation are studied and the stability of rotation is proved. A libration angle as a function of time is found using the derived solution of the differential equation. Limiting cases of infinitely large and infinitely small viscosity are considered and an effect of lag of a libration phase from a phase of action of an external moment of forces is ascertained. This makes it possible to estimate the viscosity and sizes of the lunar fluid core from data of observations.     

Calculation of the global system of the field-aligned currents on the dayside of the magnetosphere

Using the well-known equation for the normal component of the current which exist near the tangential discontinuity in the plasma in the case of the frozen-in magnetic field, and supposing that the current closes in the ionosphere in the auroral oval in the region 1, one calculates and compares with the data of observations the dependence of the density of the field-aligned current at the level of the ionosphere on the local time.     

Rotation of the elastic Earth: the role of the angular-velocity-dependence of the elasticity-caused perturbation

We calculate the so-called convective term, which shows up in the expression for the angular velocity of the elastic Earth, within the Andoyer formalism. The term emerges due to the fact that the elasticity-caused perturbation depends not only on the instantaneous orientation of the Earth but also on its instantaneous angular velocity. We demonstrate that this term makes a considerable contribution into the overall angular velocity. At the same time the convective term turns out to be automatically included into the correction to the nutation series due to the elasticity, if the series is defined by the perturbation of the figure axis (and not of the rotational axis) in accordance with the current IAU resolution. Hence it is not necessary to take the effect of the convective term into consideration in the perturbation of the elastic Earth as far as the nutation is related to the motion of the figure axis.     

Impact of the Quadrupole Moment of the Sun on the Dynamics of the Earth-Moon System

Range of values of the Sun's mass quadrupole moment of coefficient J₂ arising both from experimental and theoretical determinations enlarge across literature on two orders of magnitude, from around 10^-7 until to 10^-5. The accurate knowledge of the Moon's physical librations, for which the Lunar Laser Ranging data reach an outstanding precision level, prove to be appropriate to reduce the interval of J₂ values by giving an upper bound of J₂. A solar quadrupole moment as high as 1.1 10^-5 given either from the upper bounds of the error bars of the observations, or from the Roche's theory, is not compatible with the knowledge of the lunar librations accurately modeled and observed with the LLR experiment. The suitable values of J₂ have to be smaller than 3.0 10^-6. As a consequence, this upper bound of 3.0 10^-6 is accepted to study the impact of the Sun's quadrupole moment of mass on the dynamics of the Earth-Moon system. Such as effect (with J₂ = 5.5±1.3 × 10^-6) has been already tested in 1983 by Campbell & Moffat using analytical approximate equations, and thus for the orbits of Mercury, Venus, the Earth and Icarus. The approximate equations are no longer sufficient compared with present observational data and exact equations are required. As if to compute the effect on the lunar librations, we have used our BJV relativistic model of solar system integration including the spin-orbit coupled motion of the Moon. The model is solved by numerical integration. The BJV model stems from general relativity by using the DSX formalism for purposes of celestial mechanics when it is about to deal with a system of n extended, weakly self-gravitating, rotating and deformable bodies in mutual interactions. The resulting effects on the orbital elements of the Earth have been computed and plotted over 160 and 1600 years. The impact of the quadrupole moment of the Sun on the Earth's orbital motion is mainly characterized by variations of , , and . As a consequence, the Sun's quadrupole moment of mass could play a sensible role over long time periods of integration of solar system models. This revised version was published online in July 2006 with corrections to the Cover Date.     

On the role of the motion of the photospheric footpoints of the magnetic field lines

By means of a simple relation between the velocity v of the fluid particle and the velocity v_f of the photospheric footpoint of the magnetic field line v_z and B_z being respectively the components of v and the magnetic field B normal to the photospheric surface, it is shown formally that through the phtospheric surface the transport of all the quantities attributed to the magnetic field, such as the magnetic flux, the magnetic energy and the helicity, is independent of v_z, and v_f is the only kinematical quantity on which the transport depends. In addition, in the neighborhood of the neutral line the velocity v_l of the moving curve of constant B_z is found to be equal approximately to the component of v or v_f in the direction of v_l. Since v_l can be measured or extimated, so can the components of v and v_f near the neutral line.     

Determination of the temperature of the solar corona from the spectrum of the electron-scattering continuum

When the K-corona is formed by the scattering of photospheric radiation from free electrons, the Fraunhofer lines are greatly broadened by the thermal motions of the hot electrons. This paper discusses the possibility of measuring the coronal electron temperature from the residual depressions in the K-coronal spectrum. If the ratio of the intensities at 4100 Å and 3900 Å can be measured to an accuracy of ±1%, the coronal temperature can be inferred to an accuracy of ±0.2 MK. The temperature of a coronal inhomogeneity may also be measured by this method, provided the position angle is known.Now at Fraunhofer Institute, Freiburg, Germany.     

On the systematic errors of the determinations of the absolute orientation of the meridian marks

The classical method of determination of the absolute azimuth (or Bessel's parameter n) can secure sufficiently precision for RA from observations of stars at high geographical latitudes during polar night only.