GIS中空间数据不确定性的混合熵模型研究

基于信息理论和模糊集合理论，针对GIS中部分空间数据既具有随机性又具有模糊性的特点，建立了空间数据不确定性的混合熵模型。以GIS中线元不确定性为例，讨论了线元不确定性的统计熵、模糊熵和混合熵估计方法，并针对特例给出了线元不确定性的熵带分布。     

Instability of sand–silt mixtures

The instability of the sand–silt mixtures with different amount of fines contents were studied in this paper. It showed that the slope of the instability lines increases with the increasing relative densities, and it approaches the slope of the failure line (steady state line) at a high relative density. The relationship between the peak stress ratio and the intergranular void ratio can be described by a common curve for all the mixtures with fines contents less than the transitional fines content. There may also exist a unique curve for the relationship between the peak stress ratio and interfine void ratio for the mixtures with fines contents higher than the transitional fines content. If the yield strength ratio is used instead of the peak stress ratio, the relationships can be characterized in the same way.     

一次强飑线过程的中小尺度特征分析

通过常规资料、新一代天气雷达、自动站等资料对2005年3月22日影响福建的一次飑线系统进行分析。分析指出，该飑线系统是由高空槽前型的上干下湿引起的不稳定强对流天气。对新一代天气雷达资料分析揭示了此次飑线的典型的弓状特征、强的后侧入流槽口以及入流槽口上的弱回波区等中小尺度结构特征是造成灾害性大风的成因。     

The Work of the British Government's Air Survey Committee And its Impact on Mapping in the Second World War

It has been asserted by Clough (1952) , amongst others, that British Military Survey was poorly prepared for the outbreak of war in 1939. An examination of the work carried out between the wars by the Air Survey Committee would seem to contradict that view. In this paper, the work of the Air Survey Committee is discussed and a brief assessment made of the impact of its work on British mapping during the Second World War.     

利用精密水准及GPS数据分析中国东部地壳运动

根据现代大地测量结果及对研究区所处的构造环境的研究,本文对中国东部大陆地块地壳运动的地球动力学机制进行了探讨。通过高精度静态GPS数据处理结果验证了青藏地壳由于碰撞挤压向东挤出这一构造现象。并结合精密水准数据及研究区内的矿物、岩石、地层及地质构造特征,本文认为由于秦岭－大别构造线和郯庐断裂带是控制中国东部大陆地块运动的两条主要构造线,在郯庐断裂以东,秦岭－大别构造线经郯庐断裂转换后向北平移到青岛－五莲一带。     

A progressive line simplification algorithm

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一种有效提高DEM建模速度的方法设计及实现

文中利用动态数据链表的技术 ,为等高线数据重新设计了一种数据结构和检索方法 ,从而实现了内存中有效地操作等高线数据 ,使基于矢量等高线数据的 DEM建模速度得到了显著的提高     

面要素汉字注记自动配置的一种算法

地图注记的计算机配置是地图自动化生产、电子地图制作与显示以及地理信息系统中不可缺少的组成模块。文中着重讨论了面状要素汉字注记的原则、特点 ,对现有一些算法进行了改进 ,提出了一种面状要素汉字注记自动配置的新算法     

MHD model of magnetosheath flow: comparison with AMPTE/IRM observations on 24 October, 1985

We compare numerical results obtained from a steady-state MHD model of solar wind flow past the terrestrial magnetosphere with documented observations made by the AMPTE/IRM spacecraft on 24 October, 1985, during an inbound crossing of the magnetosheath. Observations indicate that steady conditions prevailed during this about 4 hour-long crossing. The magnetic shear at spacecraft entry into the magnetosphere was 15°. A steady density decrease and a concomitant magnetic field pile-up were observed during the 40 min interval just preceding the magnetopause crossing. In this plasma depletion layer (1) the plasma beta dropped to values below unity; (2) the flow speed tangential to the magnetopause was enhanced; and (3) the local magnetic field and velocity vectors became increasingly more orthogonal to each other as the magnetopause was approached (Phan et al., 1994). We model parameter variations along a spacecraft orbit approximating that of AMPTE/IRM, which was at slightly southern GSE latitudes and about 1.5 h postnoon Local Time. We model the magnetopause as a tangential discontinuity, as suggested by the observations, and take as input solar wind parameters those measured by AMPTE/IRM just prior to its bow shock crossing. We find that computed field and plasma profiles across the magnetosheath and plasma depletion layer match all observations closely. Theoretical predictions on stagnation line flow near this low-shear magnetopause are confirmed by the experimental findings. Our theory does not give, and the data on this pass do not show, any localized density enhancements in the inner magnetosheath region just outside the plasma depletion layer.