共查询到18条相似文献,搜索用时 526 毫秒
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1996年1月 ̄1998年3月,我们用光电方法测定了丽江高美古在B、V两个波段的大气消光系数。为便于比较,在1996年1月还测定了云南天文台凤凰山台址的大气消光系数。本文给出了观测结果,同时也列出了世界上一些天文台站的数据以供参考。 相似文献
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1996年1月 ̄1998年3月,我们用光电方法测定了丽江高美古在B、V两个波段的夜天光亮度。为便于比较,在1996年1月还测定了云南天文台凤凰山台址的夜天光亮度。本文给出了观测结果,同时出列出了世界上一些天文台站的数据以供参考。 相似文献
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1996年1月~1998年3月,我们用光电方法测定了丽江高美古在B、V两个波段的夜天光亮度。为便于比较,在1996年1月还测定了云南天文台凤凰山台址的夜天光亮度。本文给出了观测结果,同时也列出了世界上一些天文台站的数据以供参考。 相似文献
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大气消光系数的测定是天文观测台站一项很重要和基础的工作.介绍了利用新建的2.4 m望远镜在高美古观测站开展的消光系数测定等定标工作的初步结果.利用2009年4~5月对Landolt标准星场的2次测光观测,分别给出了UBVRI 5个波段的消光系数.此外,对该站点大气消光的成分情况进行了探讨.给出的结果与数年前高美古观测站选址时得到的大气消光系数基本一致,并与其它一些知名天文观测台站的消光数据进行了比较. 相似文献
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云南天文台丽江高美古和昆明的大气视宁度研究 总被引:5,自引:1,他引:4
研究云南天文台昆明凤凰山和丽江高美古两地点的大气视宁度。利用云南天文台于1994年建立的3孔较差视宁度监视仪(3孔DIMM),对这两个地点的视宁度对比观测。还利用云南天文台的1米望远镜所得到的视宁度与3孔DIMM所测的视宁度进行对比。1米望远镜和3孔DIMM同时观测了7个晚上,各取得308组数据,它们的视宁度平均分别为0.90〃和0.84〃。还讨论了3孔DIMM采用不同曝光时间对视宁度测量值的影响,从实验得出3孔DIMM采用20ms曝光比采用8ms曝光所测视宁度的值要好15%左右。从1995年5月-1996年12月,对丽江高美古和昆明凤凰山二地进行了视宁度的对比观测。在高美古和昆明分别观测了234夜和256夜,观测结果是两个点的视宁度平均;丽江为0.70〃,昆明为0.95〃,同时也统计了两个点的月平均视宁度和最好夜的视宁度,并讨论了两地视宁度随时间的变化规律。 相似文献
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In a model project unprecedented in size and scope, Academic Press has made available its 175 scientific journals to licensed
institutions in full-text over the WWW since January 1996. This article describes the unique business model behind this project,
and gives a first evaluation after one year.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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Measurements of martian atmospheric water vapor made throughout Ls = 18.0°-146.4° (October 3, 1996-July 12, 1997) show changes in Mars humidity on hourly, daily, and seasonal time scales. Because our observing program during the 1996-1997 Mars apparition did not include concomitant measurement of nearby CO2 bands, high northern latitude data were corrected for dust and aerosol extinction assuming an optical depth of 0.8, consistent with ground-based and HST imaging of northern dust storms. All other measurements with airmass greater than 3.5 were corrected using a total optical depth of 0.5. Three dominant results from this data set are as follows: (1) pre- and post-opposition measurements made with the slit crossing many hours of local time on Mars’ Earth-facing disk show a distinct diurnal pattern with highest abundances around and slightly after noon with low abundances in the late afternoon, (2) measurements of water vapor over the Mars Pathfinder landing site (Carl Sagan Memorial Station) on July 12, 1997, found 21 ppt μm in the spatial sector centered near 19° latitude, 36° longitude while abundances around the site varied from as low as 6 to as high as 28 ppt μm, and (3) water vapor abundance is patchy on hourly and daily time scales but follows the usual seasonal trends. 相似文献
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张勤 《中国天文和天体物理学报》1990,(1)
在太阳活动预报中,预报因子的选取和处理对预报效果影响甚大。本文在云台原有的平均综合指数基础上,运用模糊识别方法,给出了一种模糊识别综合指数,它能更好地表征太阳日面活动区的活动特征。这种方法简单、方便,较充分地利用了预报因子中所含有的有用信息,从而使识别预报率有所提高。 相似文献
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D. Burns J. E. Baldwin R. C. Boysen C. A. Haniff P. R. Lawson C. D. Mackay J. Rogers T. R. Scott D. St.-Jacques P. J. Warner D. M. A. Wilson & J. S. Young 《Monthly notices of the Royal Astronomical Society》1998,297(2):462-466
We report the first direct detection of long-term periodic diameter variations in a Mira variable. Angular diameter measurements of the 313-d period variable R Leonis at 833 nm and 940 nm obtained between 1996 February and 1997 June using the Cambridge Optical Aperture Synthesis Telescope (COAST) and the William Herschel Telescope (WHT) show a cyclic modulation of the apparent stellar diameter by approximately 35 per cent. The agreement between these new data and archival measurements from 1992 January suggests coherence in the modulation over a 5-yr period. Our data are consistent with recent models which suggest that, in photometric bands with only weak to moderate molecular contamination, periodic variations in stellar diameter of order 50 per cent can be maintained. The measurements indicate that the apparent stellar diameter was largest at visual phase 0.5 and that any phase shifts between the visual light curve and those at 833 and 940 nm were at most 0.05. The large offset (∼ 0.25) between the phase of the observed diameter maximum and that predicted for the photospheric continuum diameter variations suggests that our observations are more sensitive to the changing temperature structure of the outer atmosphere than to the deeper continuum-forming layers. 相似文献