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1.
讨论了产生脉冲星标准脉冲轮廓的重要性.在分析经典脉冲轮廓生成方法的基础上,提出了基于小波模极大值相关处理的脉冲轮廓累加方法.首先将观测数据按周期分组,分别进行小波分解,生成粗尺度上以脉峰为特征点的小波系数;然后,选择某组高信噪比信号的系数为参考数据,分别与其它各组变换系数进行相关,确定脉峰的相对时延.最后,对分组的原始观测数据按此相对时延量进行累加,生成脉冲轮廓.观测信号可先通过背景噪声估计和平滑处理而得到信噪比较高的归一化标准轮廓.实例分析以及与模板相关法的比较结果表明:该方法简单而有效,不需要设计近似模板,且对噪声类型不敏感,具有较高的工程应用价值. 相似文献
2.
本文根据在考虑磁光效应的条件下由斯托克斯参数转移方程组的数值解求得的斯托克斯参数轮廓,探讨V轮廓的不对称性和剩余圆偏振产生的原因,并论证白光磁象仪的工作原理。本文指出,V轮廓的不对称量与磁场强度和速度场精度都有关,因此文[1]和[4]的两个极端性论断都与实际情况不符。 相似文献
3.
根据Ｋｅｒｒ度规下粒子运动的一般方程,计算黑洞周围一般轨道单色发光环的谱线轮廓,获得了坐标系曳（ＦＤ）的特征。结果表明,原谱线发生分裂,呈现具有伴峰的双主峰轮廓,且随参数变化峰型差异明显;谱线全部发生谱移,计算参数下谱移量为负０．５到１．５;并且应用上述ＦＤ的证据,结合ＭＣＧ－６－３０－１５实际观测结果,讨论了利用发射谱线获得黑洞相关信息的可行性。 相似文献
4.
汪洵浩 《中国天文和天体物理学报》1988,(1)
近年来,谭徽松等人以所选用标准星的观测轮廓与Gray的转致轮廓直接卷积,再与被测星观测轮廓比较,由此来测量了一些恒星的自转。在这种方法中,当所选标准星自转速度不严格为零时,将引入误差。本文在标准星速度(vsini)_s较小的条件下,进行函数展开,先后给出了轮廓修正关系式R_0(λ)=R(λ)-α_2(△λ_L)_s~2R″(λ),及速度修正关系式(vsini)_0~2=(vsini)~2+(vsini)_s~2。并估算说明,当标准星速度(vsini)_s<5km/s,而被测星速度vsini>20km/s时,该误差可不考虑。 相似文献
5.
6.
本文考虑了一个有临边昏暗的球形刚体自转恒星模型,并考虑仪器轮廓是高斯曲线,计算了一系列转致轮廓与仪器轮廓的卷积。由计算结果得到了转致轮廓半强度宽PHW与卷积后轮廓半强度宽CHW的关系图,以及仪器轮廓半强度宽GHW与卷积后轮廓半强度宽CHW的关系图。表明,当RHW/GHW>2时,就半强度宽(FWHM)而言,卷积的结果使其变窄(而不是加宽);但是,这一变化不大于RHW的3％。这一结果使得在某些情况下对不同仪器上进行的恒星自转速度测量的归算变得简单。理论计算还指出,有可能利用实测的V·sin i—FWHM关系得到临边昏暗系数ε;并利用文献中的观测资料初步得到早型恒星O9.5—B9的临边昏暗系数为0.44—0.99。 相似文献
7.
首先考察了谱线形成深度理论及其在诊断太阳大气中矢量磁场分层结构方面的应用,指出了分别与贡献函数和响应函数相关的方法的优缺点,然后用理论斯托克斯轮廓观察各轮廓参量沿视线方向梯度对轮廓尤其是它的对称性和极值点的影响,在此基础上提出了基本假设使偏振辐射转移方程在极值点得到极大的简化而创立了一种不依赖形成深度理论的新方法。它由四个操作构成,将其中三个操作作循环处理便可得到位于所考虑的沿深度方向格点化的层次上的各轮廓参量及表面以下不能观测到的斯托克斯轮廓。整个推导采用层层往下递推模式,导出的结果以矢量磁场尤其是场强大小最令人满意。作者分别用理论轮廓和实测轮廓作了拟合,结果发现拟合轮廓在所利用的谱线非远线翼部分与被拟合轮廓相符较好,能导出比较复杂的磁结构。但本方法也存在导出的深度范围不广及推导表面不能精确定位等问题。 相似文献
8.
抚仙湖1 m红外太阳望远镜的重要终端之一是多通道高分辨成像系统,主要由两路宽带和一路窄带成像系统组成。目前窄带成像系统的工作谱线为Hα。主要介绍了窄带成像系统扫描轮廓的检测和修正。主要检测内容包括扫描轮廓的中心波长位置、扫描轮廓对称性、前置滤光片对扫描轮廓的影响、滤光器工作温度稳定性等问题。检测结果显示:扫描轮廓在656.281-0.15 nm到656.281+0.4 nm的范围内与理论轮廓较好地吻合,而在656.281-0.15 nm到656.281-0.4 nm的范围内明显衰减。同时轮廓中心波长位置(即强度最低点的波长位置)相对于滤光器显示的"0 nm"偏带点蓝移了0.013 nm。针对上述检测结果,将滤光器的工作温度提高了约0.3℃。在温度调整之后,扫描轮廓的整体特征不变,轮廓中心波长位置与"0 nm"偏带点偏差小于0.004 nm,同时红蓝翼对称偏带点的强度差异小于10%(对应1.8 km/s的多普勒速度测量误差)。目前可以明确,扫描轮廓的蓝翼衰减是由前置滤光片造成,对于常用工作范围(656.281±0.1 nm),可以忽略前置滤光片的影响。滤光器工作温度比较稳定,1个月内温度变化幅度的标准方差约0.001 7℃。目前,该滤光器仍存在的问题是扫描轮廓在"0 nm"偏带点略有突起,幅度在6%~8%。建议在以后的使用过程中,需要定期定量地对滤光器的扫描轮廓以及前置滤光片的透过率曲线进行检测。 相似文献
9.
耀斑谱线轮廓的不对称性是耀斑动力学过程的一个重要观测事实。本文在一定的耀斑半经验大气模型基础上,计算了不同速度模式和色球凝聚下的Ha和CaⅡK谱线轮廓,从半经验角度探讨了大气各个层次的速度对Hα和CaⅡK谱线轮廓的影响。结果表明:耀斑早期短时间的Hα蓝不对称性可由位于过渡区的色球凝聚引起;随后的红不对称性是上部色球物质向下运动的结果;而后来出现的CaⅡK不对称性特征则可由色球中、下部具有10—20km/s的向下速度来解释。 相似文献
10.
本文主要从理论上用解析方法讨论日珥视向速度随深度变化对谱线轮廓对称性的影响,得到的结论具有普遍性。第二节的分析表明,日珥的谱线轮廓可表示为二项叠加,其中第一项与源函数无关,只依赖于速度场模型,源函数分布仅通过第二项对谱线轮廓产生影响。然后在源函数不随深度变化的假定下,讨论各种速度场模型的谱线轮廓是否对称。得到的结论为:(1)常源函数与常速度场结合的谱线轮廓为对称轮廓;(2)常源函数与线性对称速度场结合的谱线也是对称轮廓;(3)常源函数与线性非对称速度场结合的谱线轮廓为不对称轮廓。最后,用数值计算对理论分析结果进行了检验。 相似文献
11.
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 相似文献
12.
B. P. Kondratyev 《Solar System Research》2013,47(1):1-10
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. 相似文献
13.
14.
M. V. Samokhin 《Earth, Moon, and Planets》1993,61(1):29-37
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. 相似文献
15.
Yoshio Kubo 《Celestial Mechanics and Dynamical Astronomy》2009,105(4):261-274
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. 相似文献
16.
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. 相似文献
17.
Wu Lin-xiang 《Chinese Astronomy and Astrophysics》1992,16(4):427-433
By means of a simple relation between the velocity v of the fluid particle and the velocity vf of the photospheric footpoint of the magnetic field line vz and Bz 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 vz, and vf is the only kinematical quantity on which the transport depends. In addition, in the neighborhood of the neutral line the velocity vl of the moving curve of constant Bz is found to be equal approximately to the component of v or vf in the direction of vl. Since vl can be measured or extimated, so can the components of v and vf near the neutral line. 相似文献
18.
L. E. Cram 《Solar physics》1976,48(1):3-19
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. 相似文献
19.
G. M. Petrov 《Astrophysics and Space Science》1991,177(1-2):269-270
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. 相似文献