自动化地理信息综合的发展现状和趋势

本文在强调地理信息综合对于开发和应用地理信息系统的必要性的同时，阐述了区分模型综合和图像综合在新环境下的实用意义，并总结了欧洲和北美地区在自动化综合研究方面所作的主要努力。通过分析现阶段综合方法和编程语言的特点，指出了现有计算机综合系统由于缺乏专家知识而存在的缺陷和局限性，并相应地介绍和讨论了知识获取和表达的几种实用方法。最后，列举了开发未来高智能自动化综合系统应当注意的问题和必须具备的条件。     

用专家系统技术实施居民地自动综合

本文主要论述了利用现有地图数据库数据，运用专家系统中产生式规则表示知识的方法，对居民地要素进行自动综合，生成小比例尺地图上居民地数据的方法。     

导线网可靠性分析和粗差探查

采用相关平差算法计算导线网中每个观测值的多余观测分量和各类观测值的内可靠性指标，按统计假设检验理论构成观测值的粗差检测统计量，经过探查指出可能含有粗差的观测值。最后给出内可靠性分析的结果，并提出导线网设计和施测要点建议     

中国的特种精密工程测量

介绍大坝变形观测、波带板激光准直系统等特种精密工程测量方法，在工程与工业建设、大型建构筑物变形观测及抗灾减灾等方面取得的成就和效益；阐述特种精密工程测量的成长道路，以及当前特种精密工程测量的热门话题与发展趋势。     

热带湿润气候中的局地天气预报

本文目的在于描述热带湿润气候中局地天气预报的各种方法。文中所给的结果在大多数情况下是可靠的。     

太原盆地震群的几个特征

在分析１９６６年—１９８５年间太原盆地发生的１４起震群序列资料的基础上。叙述了这些震群分布区的新构造特征、空间分布特征、震群活动区特征、震群迁移特征、震群的震源深度、震群所反映的现代局部应力场等。     

试析华清温泉水化观测中的干扰

对华清温泉在水化观测中的干扰因素及特征，进行了分析探讨。通过对观测资料、水文地质结构的分析，指出降水、排污、供水开采等因素，对泉点没有影响。得出只有本身不抽水时，井内形成的“滞留水”，对观测结果影响较大及Ｈｅ、Ｒｎ含量明显降低，Ｏ２含量增高，Ｎ２变化不大，ＣＯ２含量亦降低的结论。指出供电不足是形成滞留水的主要原因。     

近地大气物理现象与光电测距精度的关系

本文根据大气温度层结状态,讨论两种光电测距最佳观测时刻的理论。指出,在不稳定湍流状态下,更有利于获得高精度的观测值。     

Wind fluctuations near a cold vortex-tropopause funnel system observed by the MU radar

Vertical and temporal variations of three-dimensional wind velocity associated with an upper-tropospheric cold vortex-tropopause funnel system were observed by an MST radar in Japan (the MU radar). Marked changes of vertical velocity and horizontal wind direction were found between the inside and outside of the cold vortex. The vertical velocity activity outside the vortex was asymmetric; it was most active in a sector before the vortex. Unsaturated internal gravity waves in their generation stage contribute predominantly to the vertical velocity activity, suggesting that tropospheric occluded cyclones may be a possible source of middle-atmospheric gravity waves through the geostrophic adjustment process.     

Internal gravity wave selection in the upper troposphere and lower stratosphere observed by the MU radar: Preliminary results

Marked wavelike variations of the lower stratospheric wind observed on 7–10 May, 1985 by an MST radar in Japan (by the MU radar) are analyzed assuming that they are induced by monochromatic internal inertio-gravity waves. These variations are mainly composed of two modes (periods: 22 and 24 hours), both of which have zonal phase velocities (C _X ) slower than the mean westerly wind (). A statistical analysis of the zonal phase velocity shows thatC _X above andC _X below the tropopause jet stream, which is considered to be a vivid proof of wave selection due to the tropospheric mean flow and upward wave emission from the tropopause jet. A comparison between the MU radar results and routine meteorological observations leads to the conclusion that the marked waves appear when the jet stream takes a maximum wind speed.