我国天文气候特点及潜在（光学／红外）优良台址探讨

收集了我国１９７８－１９８６年和１９９０年，共１０年时间的１９２个地面气象站每天四次总云量的观测资料，分别计算了北京时间０８ｈ，０２ｈ和０８ｈ以及２０ｈ，０２ｈ和０８ｈ的无云概率，分析结果表明：我国所处的天文气候条件的大环境并非是世界上最好的，但在国内相对较好的区域里，精心挑同受叶形得影响形成的较好台址还是有可能的。     

中国第三次天文台选址高潮及对丽江高美古地区天文观测条件的初步估计

本文介绍了中国第三次天文台选址高潮的背景及最近这次台址调研的进展情况。天文气候条件普查的结果认为在中国挑选出受局部地形影响的较好台址是有可能的。报道了对华北和西北若干候选点进行踏勘和测量的结果。详细介绍了在滇西地区的选址普查和丽江高美古选址观测的经过。据云量和ＤＩＭＭ视宁度观测的初步结果来看，高美古是一个很有希望的潜在优良台址。     

我国天文气候特点及潜在（光学／红外）优良台址探讨

收集了我国１９７８─１９８６年和１９９０年，共１０年时间的１９２个地面气象站每天四次总云量的观测资料，分别计算了北京时间０８ｈ，０２ｈ和０８ｈ以及２０ｈ，０２ｈ和０８ｈ的无云概率。分析结果表明：我国所处的天文气候条件的大环境并非是世界上最好的，但在国内相对较好的区域里，精心挑选出受局部地形影响形成的较好台址还是有可能的。     

云南天文台三孔较差视宁度监视仪的建立

较详细地讲述了云南天文台三孔较差宁度监视仪的情况,然而,与一般天文理论和天文技术的专题研究不一样,天文仪器的研制有如说是研究,还不如说是归纳;它不是分析一个具体的沿示解决的难题,而是把许多已知的理论和技术综合起来,构成一台具体的仪器。所以,本文把许多至少是表面上互不相关的理论和技术问题归纳到一篇论文中。仪器是有许多模块组成的,为了起来逻辑性较强,我们将仪器分模块叙述,全文遵循如下顺序：     

高美古的大气视宁度

报导了2000年和2001年丽江高美古所观测的大气视宁度，文中统计了14个晚上的观测数据，得到的平均视宁度为0.97″，变化在0.73″～1.42″之间，这些视宁度值是用国际上天文台站测大气视宁度通用的DIMM方法，采用8ms单幅采样曝光取得的。本文还统计了丽江高美古1995年以来每年12月份的大气视宁度，可以看到高美古不同年份大气视宁度的部分变化情况。     

云南天文台大气视宁度观测和初步探讨

介绍了为云南丽江高美古选址点作对比的云南天文台点的大气视宁度观测统计和结果，对观测过程中的有关问题作了初步探讨。对高美古和云南天文台的１９９５年５月和１９９５年１２月２０日观测资料作了对比，结果表明：高美古选址点的视宁度明显优于云南天文台。     

微温传感器测量近地面大气湍流分布的建议

根据大气湍流温度结构函数的基本定律，推导了用于测量近地面大气湍流强度分布以及对天文视宁度贡献的关系式；提出了进行该项测量的具体方案以及数据处理过程。     

云南天文台三孔较差视宁度监视仪的建立

较详细地讲述了云南天文台三孔较差视宁度监视仪的情况,然而,与一般天文理论和天文技术的专题研究不一样,天文仪器的研制有如说是研究,还不如说是归纳;它不是分析一个具体的尚未解决的难题,而是把许多已知的理论和技术综合起来,构成一台具体的仪器。所以,本文把许多至少是表面上互不相关的理论和技术问题归纳到一篇论文中。仪器是有许多模块组成的,为了看起来逻辑性较强,我们将仪器分模块叙述,全文遵循如下顺序：１在第一篇中,回顾世界各天文台视宁度测量设备的发展史和云南天文台的宁静度测量发展史;２在第二篇中,介绍：１）云南天文台三孔较差视宁度研制任务的来源,仪器的整体状况;２）介绍云南天文台三孔较差视宁度仪的硬件系统;３）介绍云南天文台三孔较差视宁度仪的软件系统;若大模块中有多个小模块,在每一个大模块中,又遵循下述顺序：１）本模块的总体功能;２）构成该模块的基本技术;３）这些基本技术如何构成整体和完成预定功能。３在第三篇中,介绍我们所作的与视宁度测量有关的一些实验和实验结果。     

云南天文台DIMM的视宁度测量和评估

为对三孔ＤＩＭＭ数据的可靠性有进一步认识，作者对所用ＣＣＤ的曝光时间、不同大小的子瞳以及风向对观测结果的影响等方面做了试验，还进行了ＤＩＭＭ结果与一米望远镜的星像轮廓结果的比对。     

湍流大气的像质衰减参数及测量

讨论了经过大气后天文图象的象质衰减,研究了对这种衰减进行描述的宁度参数ｒ０及其它几个大气光学参数,介绍了几种测量象质衰减参数的方法,重点介绍了我们将差分像运动法运用于白日视宁度测量的尝试以及新设计的可兼顾昼夜的视宁度测量仪,仪器已用于云台白日的视宁度测量。最后对近场近似假设进行了定量分析,在此基础上给出新确定的近场近似成立的范围,这一范围比以前所给的要更大些。     

A Review of Daytime Atmospheric Optical Turbulence Profile Detection Technology

Atmospheric turbulence has been confirmed as the primary source affecting the quality of ground-based telescope image. To reduce the effect of atmosphere, a good site should be selected, and adaptive optics (AO) should be installed for the telescope. In general, the daytime atmospheric turbulence is more intense than that at night under the effect of solar radiation. Numerous solar telescopes have built AO systems worldwide. Conventional AO is only capable of improving the image quality in a small field of view, whereas it cannot satisfy the needs of a large field of view. The novel wide field adaptive optical system is capable of achieving a large field of view and high-resolution images, whereas the atmospheric turbulence profile should be accurately detected, which is the prerequisite and key parameter of the novel AO system. Moreover, the astronomical high-resolution technology in accordance with the turbulence imaging theory requires more detailed detection of turbulence. Accordingly, a brief review about the latest detection technology of the daytime optical turbulence profile is valuable for astronomical observations. Besides, the parameters of atmospheric turbulence are briefly introduced. Subsequently, SNODAR, SHABAR, MOSP, DIMM+, A-MASP, and other detection technologies of the stratified atmospheric turbulence for daytime are primarily presented, and the advantages and disadvantages of the different technologies are summarized.     

Method of Modeling Atmospheric Optical Turbulence

The intensity and distribution of optical turbulence are important parameters to evaluate an observing station. A modeling method to obtain n atmospheric optical turbulence parameters, including the C2_n pro?le, coherent length, coherent time, seeing, isoplanatic angle, and scintillation index by using meteorological parameters are presented. The accomplishment of this method, the con?guration of the WRF model (Weather Research and Forecasting Model), and the veri?cation of calculated results are introduced. The reliability of the method is con?rmed preliminarily by comparing the calculated results with the DIMM (Differential Image Motion Monitor) measurements.     

大气光学湍流模型计算方法

光学湍流的强弱和分布是描述天文台址优劣的重要参数.介绍了利用大气模式WRF (Weather Research and Forecasting Model)计算高美古站周围大气光学湍流参数的方法,这些参数包括C2n(大气光学湍流强度)廓线、大气相干长度、大气相干时间、视宁度、等晕角和闪烁率等.包括模型计算方法的实现过程、模型的设置和模拟结果的验证.计算结果与云南高美古观测站DIMM (Differential Image Motion Monitor)的实测数据进行了对比.     

天文选址定点观测中大气透明度的测量方法

本文叙述了在天文选址定点观测中使用ＵＢＶ三色光电测光系统测量大气透明度的最佳方法和所用到的各个计算公式，也包括了某些经验。     

大气湍流理论的进展及其天文学意义(英)

传统的大气湍流理论始于大约30年前．湍流理论的发展使得天文学家对大气湍流对天文观测的影响有了很好的认识，尤其是它为天文台选址和天文高分辨率技术提供了基础．近年来新的天文观测已对传统的大气湍流理论提出了挑战，并可能给地面天文观测带来一场革命．在回顾了大气湍流理论的发展历史后对传统大气湍流理论的基本特性及其应用作了系统的综述，并介绍了新的天文观测事实以及为此而提出的新的大气湍流理论模型．     

Gulmarg,Kashmir, India: Potential Site for Optical Astronomical Observations

The site characteristics of Gulmarg, Kashmir at an altitude of about 2743.2 m above sea level is based on analysis of meteorological conditions, cloud cover, temperature, wind speed, wind direction, relative humidity and atmospheric pressure, etc. Analysis and characterization of meteorological conditions suggest that Gulmarg, Kashmir is a potential site for carrying out photometric as well as spectroscopic observations of celestial objects.     

On Astronomical Atmospheric Refraction

Through a comparison between the series expression and mapping function expression of the astronomical refraction, we believe that, as far as a specific atmospheric refraction model is concerned, the computational accuracy is not lower in the former than in the latter, and that the convergence is poorer in the theoretically derived series expression, because of the different approximations made. From an analysis of the method of generating function of the atmospheric refraction mapping function it is considered that this kind of method can not embody the characteristics of geophysics and atmospheric physics. It is pointed out from the comparison that the atmospheric refraction model which is constructed by adopting the specific atmospheric distribution of a certain place does not apply to all other places and cannot be used to evaluate the other atmospheric refraction models. For improving the correction accuracy the key lies in the adoption of an effective method by which the instantaneous refraction values at different positions are directly determined to construct a local, position-dependent model of atmospheric refraction observation.     

天文选址中的地理信息处理

地理信息是地面望远镜天文选址研究中的重要内容.尤其是对现有地理信息系统(Geographic Information System,GIS)的有效利用,已成为现代选址中远程分析阶段最重要的手段之一.天文址点的考虑在地理条件上应遵循以下原则:相对落差较大、交通可行、尽量远离人口集中的区域.从未来建站维护和人员长期驻站的角度考虑,天文址点以海拔处于3000～5000 m的范围、距离城镇大本营1 h左右车程为最佳.以云南省大姚县百草岭地区为选址研究对象,展示了GIS数据处理能够为全面了解一个候选区域3维地形地貌、江川河流、道路村落、电力分布以及预测该地区未来人口和城市化发展趋势等方面内容提供准确、直观、定量的参考数据.通过基于GIS数据的科学分析,发现海拔3 600多米的大百草岭山顶平坦而又干旱、周围人口稀少、道路便利、无工厂污染源,是地方政府重要自然保护区;它与直线距离10 km外的乡镇之间的相对落差超过了1 500 m,与50km外的县城的相对落差达到1 800 m,是滇中彝州坝区一座名副其实的孤峰.因此,GIS数据分析对于远程选址十分有益,GIS技术是现代天文选址不可或缺的重要手段.     

天文选址相机的研制

详细介绍了天文选址用CCD相机的开发研制．系统探测器选用具有累进扫描模式的ICX098ALCCD芯片，采用相关双采样信号读出电路、USB通讯接口实现数据与命令的传输．对系统工作性能进行了详细的测试：12℃条件下暗流约为52adu／see，系统增益(system gain)为2.2e／adu，读出噪声(readout noise)为30e．最后给出了在日本冈山天体物理观测所对大气宁静度的实测结果，该结果与冈山已有仪器测量值吻合．     

Processing Method of Night-Time Cloudiness for Astronomical Site Selection

The cloudiness is one of the most important factors which affect the quality of an astronomical site, the monitoring and processing of the night- time cloudiness are especially important. The ground-based cloudiness camera is adopted to carry out the monitoring of the all-sky cloudiness, the images taken need to be processed by means of an effective method so as to quantize the cloudiness. The night-time cloudiness images are seriously affected by the moon- light, and therefore, the night-time cloudiness images are processed by dividing them into the moonlight and moonless two sorts. In the light of the condition of moonless night, the processing method of night-time cloudiness is given. The positioning and photometry of the bright stars in the image are conducted to determine their magnitude differences. By referring to the magnitude differences of the bright stars in the clear-night image, the probability of the bright stars of which the magnitude differences are lower than the threshold value are regarded as the probability standard of clear nights. Three sorts of images are selected to test the method. The cloudiness is determined, and the effect of the threshold condition on the result is analyzed. Finally, the applicable range and uncertainty of the method are discussed.