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1.
观测角     
观测角土里冲日9月15日22时22分土星冲日。在这前后的几个月里,是今年观测土星的最佳时期。1995年全年,土星一直在宝瓶座中,7月7日和11月22日两次日之间,上星送行,其余时间顺行。冲日对土星位置为赤经23‘32”,赤纬一5”.6,星等十0.7等...  相似文献   

2.
我看到了水星凌日水星凌日是水星经过日面的天文现象,平均每一百年发生十三次。本世纪最后两次水星凌日是在1993年11月6日和1999年11月15日发生。11月3日,我收到载有水星凌日资料的《业余天文快讯》,并参考《天文爱好者》和《天文普及年历》,计算了...  相似文献   

3.
CSRH模拟接收机设计   总被引:1,自引:1,他引:0  
本文叙述了日像仪实验的方案,双天线干涉仪中模拟接收机的结构,灵敏度,动态范围,噪声,增益的各级分配等问题,基于实验方案设计了日像仪模拟接收机。  相似文献   

4.
我国雷暴活动对太阳耀斑响应的东西不对称性   总被引:3,自引:0,他引:3  
傅元芬  陈济民 《天文学报》1997,38(3):264-272
本文研究了1971—1980年间发生在日面东部的164个和西部的132个2级以上耀斑对我国185个气象站上空雷暴活动的影响.结果表明,日面东部耀斑爆发后雷暴活动减弱且通过优于0.1的置信度检验测站数远多于日面西部耀斑,而日面西部耀斑爆发后雷暴活动增强,通过优于0.1的置信度检验测站数远多于日面东部耀斑.这种与地磁活动和日球扰动相似的雷暴活动对太阳耀斑响应的东西不对称性,可能借助于大气电环境并通过行星际磁场和磁层,将太阳和对流层的确耦合起来了.  相似文献   

5.
利用色球Hα、TRACE/WL、SOHO/EITEuV单色像观测资料及SOHO/MDI光球磁场观测资料,对2003年10月22日太阳活动区AR0484内发生的日浪事件进行了研究.发现:(1)在Ha线心观测上,日浪包含有亮、暗2个分量,这2个分量先后出现而且并不共空间.日浪的亮分量与UV和EUV波段上观测到的喷发具有较好的同时性和共空间性.(2)日浪喷发物质沿着EUV环运动。(3)在光球层,日浪足根处的黑子和磁场有明显的变化.这些观测结果支持日浪的磁重联模型。  相似文献   

6.
本文研究结果表明:同一黑子群在日面期间的顺或反时针方向的旋转运动会先后并存.质子耀斑前1~2无,黑子群的旋转角速度达到极大.耀斑后,磁绳的松弛,黑子群可能会反向旋转,强的剪切过程和质子耀斑可能会再度出现.强质子耀斑活动区的共同特征是:(1)形态为单个团状结构δ型黑子,即众多异极性本影核紧锁在同一黑子半影中;(2)黑子面积>1000×10-6半球面积,日面跨度>10°;(3)黑子群都有快速的旋转运动.这类活动区,如果在日面西部活动性明显地增强,那么这个活动区在未来转到日面边缘及其背后、或再次从日面东边缘转出时,定能再次爆发耀斑和伴随较强质子事件。  相似文献   

7.
月初,太阳的视赤纬为十4”34’.0:月末,太阳的视赤纬为十14”47’.5。本月太阳由双鱼座运行至白羊座。4日20时02分清明,太阳的黄经为15”。20日3时10分谷雨,太阳的黄经为30”。月亮过近地点、远地点的时间分别为11日门时、25日6时。月...  相似文献   

8.
有关天文的节日太阳节从1977年起,墨西哥在全国技术研究所的倡议下,每年3月20日举办太阳节。节日期间,展出利用太阳能和观测太阳的新成果。月亮节1967年7月16日,美国成功地发射了“阿波罗一11号”宇宙飞船,并于7月20日下午,首次完成了人类登月壮...  相似文献   

9.
简讯     
简讯全国各省市和田开展“天文日”科苦活动为提高全社会学科学爱科学的意识,促进天文科普工作,中国天文学会普及工作委员会决定将每年的10月30日定为“全国天文日”,号召各地方积极开展天文科普活动。为此,今年各省市有关部门举办了形式多样丰富多采的天文科普活...  相似文献   

10.
1997年3月9日在云南天文台对日偏食进行了光学观测,取得了不同时刻的日面掩食过程的白光资料,是射电等观测分析研究的重要依据  相似文献   

11.
木星探测轨道分析与设计   总被引:3,自引:0,他引:3  
研究了与木星探测相关的轨道设计问题.重点关注木星探测轨道与火星、金星等类地行星探测轨道的不同及由此带来的轨道设计难点.首先分析了绕木星探测任务轨道的选择.建立近似模型讨论了向木星飞行需要借助多颗行星的多次引力辅助,对地木转移的多种行星引力辅助序列,使用粒子群算法搜索了2020年至2025年之间的燃料最省飞行方案并对比得到了向木星飞行较好的引力辅助方式为金星-地球-地球引力辅助.结合多任务探测,研究了航天器在飞向木星途中穿越主小行星带飞越探测小行星的轨道设计.最后,给出2023年发射完整的结合引力辅助与小行星多次飞越的木星探测轨道设计算例.  相似文献   

12.
Trajectory Analysis and Design for A Jupiter Exploration Mission   总被引:1,自引:0,他引:1  
The trajectory design for a Jupiter exploration mission is investigated in this paper. The differences between the Jupiter exploration trajectory and the Mars or Venus exploration trajectory are mainly concerned about. Firstly, the selection of the Jupiter-centered orbit is analyzed based on the Galileo Jupiter mission. As for the Earth-Jupiter transfer orbit, the fuel consumption of the direct transfer is too large. So the energy-saving technologies such as the planetary gravity assist should be used for the trajectory to the Jupiter. The different sequences of planetary gravity assists are examined by applying the Particle Swarm Optimization (PSO). According to the searched result, the Venus-Earth-Earth sequence (VEEGA) is the most effective one for the Jupiter mission. During the Jupiter mission, the spacecraft will pass though the main asteroid belt between the orbits of Mars and Jupiter, and may encounter multiple asteroids. Therefore the Jupiter mission is able to combine with the main-belt asteroid flyby mission. The design method of the intermediate asteroid flyby trajectory is also considered. At last, an entire trajectory for the Jupiter mission launched in 2023 is presented.  相似文献   

13.
《Planetary and Space Science》1999,47(10-11):1201-1210
New models of Jupiter are based on observational data provided by the Galileo spaceprobe, which considerably improved previously existing estimates of the helium abundance in the atmosphere of Jupiter. These data yield for Jupiter’s atmosphere 20% of the solar oxygen abundance and do not agree with the results of the analysis of the collision of comet Shoemaker-Levy 9 with Jupiter (10 times the solar value). Therefore, both the models of Jupiter with water-depleted and water-enriched atmosphere are considered. By analogy with Jupiter, trial models of Saturn with a water-depleted external envelope are also developed. The molecular-metallic phase transition pressure of hydrogen Pm was taken to be 1.5, 2 and 3 Mbar. Since Saturn’s internal molecular envelope is noticeably enriched in the IR-component (its weight concentration, 0.25–0.30, being by a factor of 3–4 higher than in Jupiter), the phase transition pressure in Saturn can be lower than in Jupiter. In the constructed models, the IR-core masses are 3–3.5 M for Jupiter and 3–5.5 M for Saturn. Jupiter’s and Saturn’s IR-cores can be considered embryos onto which the accretion of the gas occurred during the formation of the planets. The mass of the hydrogen–helium component dispersed in the zone of planetary formation constitutes ≈2–5 planetary masses for Jupiter and ≈11–14 planetary masses for Saturn.  相似文献   

14.
Jupiter‐family comets (JFCs) may often, closely and/or slowly approach Jupiter. A list of their close approaches within 0.21 AU from Jupiter between 1970 and 2030 is presented to determine the typical changes in some of their orbital elements and their relation to any triggered activity. A few JFCs from the list were temporary satellites of Jupiter. There are also several JFCs which originally had asteroidal provisional designations due to their low activity at discovery. But Jupiter is also approached by asteroids. The presented list of their approaches within 0.60 AU from Jupiter between 1960 and 2040, together with their orbital changes can be compared with the list of comets. Some of the orbital changes are large enough to cause an extremely low or short‐lived activity. Usually, quick and dedicated observations by large‐aperture telescopes are missing to confirm or refute it. Currently, the most important cometary candidate among Jupiter approaching asteroids is 2004 FY140. (© 2005 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

15.
Maps of Jupiter at 5 um provide detailed information about the complex of emission features at this wavelength. Previous indications of a correlation between infrared sources and visual features are confirmed with a few significant exceptions. The behavior of Jupiter at 5 um is compared with that of other bodies in the outer solar system. Recent observations indicate emission features on Jupiter at other infrared wavelengths.  相似文献   

16.
The sets of photographic observations of the Galilean satellites of Jupiter taken at the Abastumani Astrophysical Observatory of the Academy of Sciences of Georgia are analyzed here. Positional observations of the system of Jupiter were made in the period from 1985 to 1994 with the use of the double Zeiss astrograph in order to determine the exact coordinates of Jupiter and its satellites. The accurate positions of the satellites and Jupiter itself, as well as their stellar (equatorial) coordinates relative to the stars of the currently available catalogs and the relative ??satellite ?? satellite?? coordinates were obtained from the observations. From the comparison of the observation results with the modern theories of motion of satellites, the accuracy in determining the positions of the satellites and Jupiter was analyzed. The results of observations are presented in the Pulkovo database of observations of Solar System bodies that is accessible to users at http://www.puldb.ru.  相似文献   

17.
Filtergrams of high spatial and temporal resolution were obtained in the methane band centred at 892 nm during the impact of fragment L of comet Shoemaker-Levy 9 on Jupiter. The light curve shows two maxima of an emission ball observed above the limb shortly after the impact. The second maximum was the brightest and had a short life time of about 90 seconds. During it's life, the apparent height of the emission ball declined towards the surface of Jupiter; the amount of displacement is larger than the expected effect caused by Jupiter's rotation. About half an hour after the impact, a domelike feature became visible when the location of the impact rotated into the illuminated hemisphere of Jupiter.  相似文献   

18.
The giant planetary magnetospheres surrounding Jupiter and Saturn respond in quite different ways, compared to Earth, to changes in upstream solar wind conditions. Spacecraft have visited Jupiter and Saturn during both solar cycle minima and maxima. In this paper we explore the large-scale structure of the interplanetary magnetic field (IMF) upstream of Saturn and Jupiter as a function of solar cycle, deduced from solar wind observations by spacecraft and from models. We show the distributions of solar wind dynamic pressure and IMF azimuthal and meridional angles over the changing solar cycle conditions, detailing how they compare to Parker predictions and to our general understanding of expected heliospheric structure at 5 and 9 AU. We explore how Jupiter’s and Saturn’s magnetospheric dynamics respond to varying solar wind driving over a solar cycle under varying Mach number regimes, and consider how changing dayside coupling can have a direct effect on the nightside magnetospheric response. We also address how solar UV flux variability over a solar cycle influences the plasma and neutral tori in the inner magnetospheres of Jupiter and Saturn, and estimate the solar cycle effects on internally driven magnetospheric dynamics. We conclude by commenting on the effects of the solar cycle in the release of heavy ion plasma into the heliosphere, ultimately derived from the moons of Jupiter and Saturn.  相似文献   

19.
X-ray fluxes at Earth estimated from hypothetical fluxes and spectra of energetic particles trapped in Jupiter's magnetic field are found to be 1/170000 times the upper limit X-ray flux from Jupiter based on published results from a rocket experiment. Detection of the calculated X-ray flux from Jupiter does not necessarily provide information on an energetic trapped proton component because the X-ray flux due to the hypothetical trapped energetic proton fluxes alone is comparable in magnitude to that due alone to trapped energetic electron fluxes at Jupiter.  相似文献   

20.
The near-infrared (0.65–2.5μm) spectral albedo of Jupiter and Saturn with 1.5% spectral resolution is presented for the center of disk and for the limb. There is a distinct difference in the continuum slope between Jupiter and Saturn which may be attributed to a difference in the dust content or composition of the two atmospheres. There is an indication of limb brightening in the deepest CH4 bands on Saturn. No limb brightening is found for Jupiter.  相似文献   

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