排序方式: 共有85条查询结果,搜索用时 287 毫秒
1.
介绍了云南天文台天体测量工作的发展过程,论述了在空间时代地面光学基本天体测量的必要性和应具备的条件,并且叙述了在新的要求和条件下,地面光学基本天体测量工作应该发挥的作用和广阔的发展前景。 相似文献
2.
A.?BoattiniEmail author G.?D’Abramo H.?Scholl O.?R.?Hainaut R.?West G.?Hahn R.?Michelsen G.?Forti P.?Pravec G.?B.?Valsecchi 《Earth, Moon, and Planets》2003,93(4):239-248
We have used the ESO Very Large Telescope (VLT) to perform as trometric observations of Near Earth Asteroids (NEAs) having
remote collision possibilities with the Earth. The observations were made for those objects which became too faint to be observed
elsewhere. Using the 4 hours allocated in the semester April–September 2003, 5 faint NEAs were observed. As a result, no NEA
that could impact the Earth was lost. 相似文献
3.
A new protocol was devised to improve the efficiency of astrometric follow-up observations of Near Earth Asteroids for the
accurate determination of their orbits. It was implemented in the activities of the Spaceguard Central Node (SCN, a facility
of the Spaceguard Foundation, established with the support of the European Space Agency) in the form of a Priority List. Here
we describe this protocol and results obtained during five years of activity (2000–2004). 相似文献
4.
5.
针对空间大地测量技术对中性大气折射延迟改正精度的要求,阐述了折射延迟改正值应随测站和随方位而异的必要性.指出,在尚不能直接测定天文大气折射值的情况下,现有的各种改正模型对大气分布模型的依赖性,不能达到预期的精度和降低观测的截止角.根据云南天文台低纬子午环的特殊结构,和测定大气折射的实践,提出了提高折射延迟改正精度的新方法,即:利用各观测站不同方位从天顶附近直到低地平高度角的天文大气折射实测数据,求解得到折射率差和映射函数的参数,从而建立随测站和随方位而异的大气折射延迟改正模型.这一新方法的实施,将能在不需采用大气分布模型的情况下,把天顶延迟的改正精度提高到1 mm以内,低地平高度角的折射延迟改正精度提高到厘米级,并且把截止高度角压缩到5°以内. 相似文献
6.
1997年11月14日晚,在中国科学院云南天文台1米望远镜上用新安装的10242CCD观测到了木星的两颗伽里略卫星;Europa和Callisto及一颗依巴谷星(星号为 104297).当采用新的 JPL DE405和 Sampson-Lieske理论(G5)计算卫星的理论位置并相对于Callisto测量恒星位置时,视位置的观测值与计算值之差的平均值在赤经和赤纬方向分别为△α=-0″029±0.″012,△δ=0.″005± 0.″011.这对应于平均观测历元(UT):1997年11月14日13时43分50秒.这一试验结果与 Casas等在同一时期内CCD观测的结果有着很好的一致性 它反映了依巴谷星表体现的光学参考系与DE405体现的动力学参考系在观测历元具有较好的一致性.单次位置测定的标准误差在赤经赤纬方向分别为±0.″052和0.″047.这一精度明显优于 Casas等人发表的 Callisto的处理精度,并与目前国际上最好的伽里略卫星观测精度相当 相似文献
7.
8.
At Beijing Observatory both astrometric and gravimetric observations are available to study the non-tidal variations in the deflections of the vertical (or non-tidal plumbline variations, PLVs). From repeated gravimetric observations performed in a network around the observatory, the PLVs at Beijing Observatory during the period 1987.0–1996.0 have been calculated. After comparison with the observational residuals (which also contain the PLV components) of the photoelectric astrolabe located at the observatory, the accuracy of the obtained PLV results has been examined. It is shown that, due to the asymmetry of the gravimetric network, the qualities of the two different PLV components are not equal. The longitude component of the PLV at Beijing has been determined successfully, to be of the order of 0.05, with a contribution of about 0.02 in the inter-annual time scale. The result for the latitude PLV component is not good enough to draw a conclusion. Although both techniques are able to measure the PLV, the result of the determination depends very much on the availability of observational data. 相似文献
9.
10.