1989年8月17日耀斑环的视向速度场

“多云模型”是处理太阳活动体光变谱不对称轮廓的有效方法,本给出了该方法的一个具体应用实例,利用云南天台二维多波段太阳光谱仪观测的１９８９年８月１７日耀斑Ｈβ波段光谱资料,得到了该耀斑环的视向速度场。     

1989年8月17日太阳边缘耀斑和速度场研究

本文利用云南天文台二维光谱仪观测的１９８９年８月１７日耀斑的Ｈβ波段光谱资料，采用多云模型的方法，得到此耀斑的观测视向速度分布，并在一定的简化和假设下，采用ＭＨＤ理论计算了几种情况下耀斑环内物质运动的视向速度分布，与观测的视向速度分布加以比较，研究和探讨耀斑环中的物质运动情况。通过分析比较，得出此耀斑环内物质运动可能属于下述两种模式：物质从环顶沿两环腿螺旋下落和物质从环足沿一环腿螺旋上升到环顶后沿另一腿螺旋下落     

1984年2月18日环状日珥和速度场

本文给出1984年2月18日耀斑后环的Hα色球和Hα-SSHG的光谱形态分析,同时给出它的二维视向速度场,并对该速度场特征给予定性解释。结果表明:(1)该环珥是一个耀斑后的拱廊(‘Post’-Flare Arch);(2)用环顶物质在重力和磁应力作用下主要沿光学厚环腿下落的假设能很好地解释观测结果。     

冕环与太阳耀斑的形成

本文讨论近年来在通过冕环相互作用而形成太阳耀斑的研究上所取得的进展。在观测上,无论在射电波段,或者X射线和光学波段的观测都提供了一些可靠的证据,说明耀斑冕环的相互作用可能导致耀斑的产生。在理论上,等离子体环的相互作用所引起的结合不稳定性将触发耀斑,释放大量的能量以产生观测到的各种辐射特性。     

1993年10月2日耀斑的Hα,微波和硬X射线暴的综合分析

本文介绍1993年10月2日发生的一个1N／C6.5级耀斑多波段观测的结果．综合比较了耀斑的单色象，Hα波段工维光谱，2840兆赫微波爆发和硬X射线爆发资料．得到Hα单色象上不同亮核的强度变化，与微波及硬X射线暴的时间轮廓比较，给出了色球耀斑区亮度场的演化，对照磁图确定了耀斑区的磁场位形，从而对该耀斑产生和加热提出了一种可能的解释．     

1986年2月4日耀斑与电流环合并不稳定性

本文收集了１９８６年２月４日大耀斑的Ｈα、微波、Ｘ射线和γ射线全波段的观测资料。利用暗条电流环模型分析了该耀斑的物理过程，测量了活动暗条的上升运动，求解了动量方程和能量方程。结果表明：（１）１９８６年２月４日的３Ｂ／Ｘ３耀斑可能是由暗条电流环之间的合并不稳定性所致；（２）电阻撕裂摸不稳定性是一种有效的耀斑前预热机制；（３）耀斑的高能观测资料进一步表明了电流环合并不稳定性是引起该大耀斑期间所有高能粒     

1991年10月24日白光耀斑的高时间分辨率多波段光谱分析

本分析了南京大学太阳塔１９９１年１０月２４日用多波段光谱仪观测到的高时间分辨率（５ｓ）的一个２Ｎ／Ｘ２．１级白光耀斑光谱，对耀斑谱线轮廓，连续发射强度，Ｘ射线和射电爆发资料进行了综合对比，分析表明，该耀斑属Ｉ类白光耀斑，具有如下特征：（１）在白光耀斑的脉冲相期间，各波段光谱线心强度，连续辐射，谱线半宽以及线翼红不对称性与硬Ｘ射线高能波段的爆分同时达到极大；（２）Ｈα谱线在连续发射极大时半宽达１０     

一个边缘耀斑(后)环系速度场的近似计算

利用“多云模型”方法,从云南天文台二维多波段太阳光谱仪观测到的Ｈβ光谱资料中导出１９８９年８月１７日太阳西边缘的一个大的耀斑环系不同时间的视向速度场．为了解释观测速度场的主要特征,本文采用如下假设和近似：环内物质在太阳重力、磁场应力和环内气压梯度力联合作用下由环足沿螺旋磁力线上升运动．应用ＭＨＤ理论计算了它的理论速度场．通过两者的比较发现,计算出的速度场与第一时段的观测速度场基本相似,这似乎对耀斑物质蒸发模型提供了支持．     

圆面耀斑环物理量场的归算和分析

本文对云南天文台1981年5月16日3B级双带大耀斑环(0922UT)的H_α—SSHG光谱资料作了初步的数据处理。采用非线性函数的最小二乘曲线拟合方法,从光谱轮廓求得圆面耀斑环的线心光学厚度τ_0、Doppler宽度Δλ_D平均能源函数S_λ及视向速度V_(11)的二维分布,为处理具有时空序列的光谱资料提供了一种数值方法。计算结果表明,耀斑环系内的物质由环顶沿两环腿向色球层溅落;用色球蒸发模型解释环中的物质来源较为合理。     

紫台多波段耀斑光谱观测

我们用紫台多波段太阳光谱仪进行耀斑光谱观测。这架仪器能在Hα、D、M_g、H_β、H_γ、H、H_δ——K、H_θ——H_(12)和H_(13)——H∞等九个波段基本上同时拍摄耀斑光谱。太阳像直径为11.2厘米,二级光谱的实测分辨率约10万,线色散度约为1毫米/埃。在这次峰年期间,从1980年2月至1981年5月,我们一共拍到16套耀斑光谱底片。我们已开始用这些资料来研究,(1)耀斑的能量传输机制,(2)耀斑的热动平衡偏离,(3)地面与空间观测资料的配合,(4)形态研究,并已开始归算处理这些资料。     

Acceleration of Numerical Integration of the Equations of Motion of Asteroids

Solar System Research - Finding and studying possible collisions of asteroids approaching the Earth requires a significant amount of computation. This paper describes the R0 program created to...     

Observations of the intensity of the penumbra of sunspots

Observations of the penumbral intensity of sunspots in 13 wavelength regions are presented. In 4 wavelength regions 54 sunspots are measured. In the other wavelength regions the number of sunspots considered ranges from 3–19.The penumbral intensity alters with position within the spot. This intensity variation is found to be comparable with the change in intensity from one spot to another. The penumbral intensity is found to be independent of spot size in the sample considered.The penumbra model of Kjeldseth Moe and Maltby (1969) with = 0.055 is supported by the measurements.     

Equation of state and anisotropy of pressure of magnetars

Magnetars are the neutron stars with the highest magnetic fields up to 10¹⁵–10¹⁶ G. It has been proposed that they are also responsible for a variety of extra-galactic phenomena, ranging from giant flares in nearby galaxies to fast radio bursts. Utilizing a relativistic mean field model and a variable magnetic field configuration, we investigate the effects of strong magnetic fields on the equation of state and anisotropy of pressure of magnetars. It is found that the mass and radius of low-mass magnetars are weakly enhanced under the action of the strong magnetic field, and the anisotropy of pressure can be ignored. Unlike other previous investigations, the magnetic field is unable to violate the mass limit of the neutron stars.     

A survey of orbits of co-orbitals of Mars

Many asteroids with a semimajor axis close to that of Mars have been discovered in the last several years. Potentially some of these could be in 1:1 resonance with Mars, much as are the classic Trojan asteroids with Jupiter, and its lesser-known horseshoe companions with Earth. In the 1990s, two Trojan companions of Mars, 5261 Eureka and 1998 VF₃₁, were discovered, librating about the L₅ Lagrange point, 60° behind Mars in its orbit. Although several other potential Mars Trojans have been identified, our orbital calculations show only one other known asteroid, 1999 UJ₇, to be a Trojan, associated with the L₄ Lagrange point, 60° ahead of Mars in its orbit. We further find that asteroid 36017 (1999 ND₄₃) is a horseshoe librator, alternating with periods of Trojan motion. This asteroid makes repeated close approaches to Earth and has a chaotic orbit whose behavior can be confidently predicted for less than 3000 years. We identify two objects, 2001 HW₁₅ and 2000 TG₂, within the resonant region capable of undergoing what we designate “circulation transition”, in which objects can pass between circulation outside the orbit of Mars and circulation inside it, or vice versa. The eccentricity of the orbit of Mars appears to play an important role in circulation transition and in horseshoe motion. Based on the orbits and on spectroscopic data, the Trojan asteroids of Mars may be primordial bodies, while some co-orbital bodies may be in a temporary state of motion.     

Graphical representation of periodic motion of the line of nodes of the Moon

In the text-books of astronomy, sections generally related to the Moon deal with the orbital elements of the Earth-Moon system such asa, e, i, , and the time of perigee passage. While the MEAN of the first of the three elements do not vary, mean longitude of the ascending node-mean longitude of the lunar perigee and the time of perigee passage undergoes secular as well as periodic changes due predominantly to the action of the Sun's gravitational attraction. While to a certain degree, explanations related to the calculation of the lunar orbit parameters are given, not a single graphical representation of these short- or long-periodic changes are presented. We allow the number of data related to these periodic changes must cover a large span of time; and if regression of the line of nodes or advances of the line of apses are to be graphically seen, data covering 18.61 and 8.85 yr, respectively, are needed. In this work we particularly aim at the graphical representation of the periodic changes of the line of nodes.