实时交通数据支持下的医疗服务时空可达性分析

针对现有城市医疗服务可达性分析方法未考虑就医偏好,导致测算结果与居民实际感受相差较大的问题,本文提出了一种顾及时间和距离成本偏好的医疗服务时空可达性分析方法,并以武汉市中心城区为例进行了分析。试验结果表明,研究方法充分利用交通路况,兼顾了交通距离和通行时间对就医选择的影响,距离偏好在新方法中作用显著。该方法一方面可以体现不同时刻可达性差异,另一方面又强调了居民就医的时间和距离成本偏好,相比单一的时间或距离成本更具优势,分析结果更符合现实。     

福建省GPS基准站数据处理与分析

利用福建省41个GPS基准站2011—2014年的观测资料,运用GAMIT／GLOBKl0．4软件及块体整体旋转线性应变模型,得到了福建省各测站及分块的水平运动速度场和块体上的应变图像。通过分析研究2011—2013和2011-2014两个时段速度场和应变场的特征,为福建省未来地震活动判定提供形变依据。     

顾及有效区域的Voronoi图的正射影像拼接

无人机影像的重叠度通常较大(60%~80%),对纠正后的正射影像进行拼接处理时,往往会产生很大的数据冗余。同时,影像越靠近边缘处变形越大,影响拼接精度。提出了一种顾及有效区域的Voronoi图的拼接线自动选取方法,基于整体构建拼接线网络,并根据影像有效区域优化拼接线,保证拼接的精度和效率。实验表明,该方法切实可行。     

人机交互策略在GIS软件用户界面设计中的研究

随着计算机技术的不断进步,用户界面设计---有效的人机交互策略变得更加重要。地理信息系统的发展要求其系统软件的设计者与开发者设计开发出更加人性化的用户界面,以提高不同领域、不同层次软件使用者的满意度。     

地理国情监测在城市化发展中的应用研究——以汕头市为例

开展地理国情监测工作的目的是为了获取自然与人类社会经济活动引起的地表变化信息,为政府、企业和公众提供地理国情信息服务。城市化发展、变迁是地理国情监测的重要应用方面之一,本文以广东省汕头市为例,基于遥感技术（ RS）,利用多时相影像数据提取不同时期建成区变化信息,并有针对性地对比分析,直观反映了汕头市三十多年的城市化发展的特点和进展情况。     

EGM2008的高程拟合模型在广西区域的应用研究

利用广西2013年测量的部分二等水准测量成果,对EGM2008地球重力场模型1′×1′的模型进行检核,得到其在广西境内的高程异常差值为36.8cm。并选取了广西两个较有代表性区域的数据,使用多种G P S高程多项式拟合的方法以及基于EGM2008地球重力场模型的移去-恢复法进行实验研究,通过数据统计分析,最优拟合模型精度可达到5cm以内,对EGM2008地球重力场模型在广西的实际应用得到了一些非常有意义的结论。     

一种基于GEO星间链路的导航系统时间同步新体制

设计提出了一种时间同步新体制即在GEO卫星上放置高精度氢钟并在GEO卫星间建立高精度星间链路以进行高精度时间维持利用两种方案进行了仿真比较研究 仿真结果表明本文提出的方案切实可行可以显著提升时间同步精度尤其是自主时间同步精度并得出了时间同步精度与星间链路精度和星载钟的精度关系 仿真结果表明星载钟精度对新体制时间同步精度的影响相对于星间链路精度的影响较小.     

快速城市化地区建设用地演变驱动力研究——以深圳市龙岗区为例

在综述国内LUCC驱动力研究的基础上,确定了驱动因子。以深圳市龙岗区为例,基于非线性的Lo-gistic模型,分析研究了建设用地演变的驱动力。     

Non-stationary covariance function modelling in 2D least-squares collocation

Standard least-squares collocation (LSC) assumes 2D stationarity and 3D isotropy, and relies on a covariance function to account for spatial dependence in the observed data. However, the assumption that the spatial dependence is constant throughout the region of interest may sometimes be violated. Assuming a stationary covariance structure can result in over-smoothing of, e.g., the gravity field in mountains and under-smoothing in great plains. We introduce the kernel convolution method from spatial statistics for non-stationary covariance structures, and demonstrate its advantage for dealing with non-stationarity in geodetic data. We then compared stationary and non- stationary covariance functions in 2D LSC to the empirical example of gravity anomaly interpolation near the Darling Fault, Western Australia, where the field is anisotropic and non-stationary. The results with non-stationary covariance functions are better than standard LSC in terms of formal errors and cross-validation against data not used in the interpolation, demonstrating that the use of non-stationary covariance functions can improve upon standard (stationary) LSC.     

Advances in understanding of the mechanism for generation of earthquake thermal precursors detected by satellites

Stresses building up during an earthquake preparation phase also manifest themselves in the form of a so called increased land surface temperature (LST) leading to a thermal precursor prior to the earthquake event. This phenomenon has now been validated by our observations of short-term thermal anomalies detected by infrared satellite sensors for several recent past earthquakes around the world. The rise in infrared radiance temperature was seen to vary between 5 and 12 °C for different earthquakes. We discuss in this paper different explanations for the generation of such anomalies that have been offered. Emission of gases due to the opening and closure of micropores upon induced stresses and also the participation of ground water have been propounded as a possible cause for generation of thermal anomalies. Seismo-ionosphere coupling, by which gases like radon move to the earth–atmosphere interface and cause air ionization thus bringing about a change in air temperature, relative humidity, etc., has been put forth by some workers. A mechanism of low frequency electromagnetic emission was tested and experimented by scientists with rock masses in stressed conditions as those that exist at tectonic locations. The workers proposed the positive hole pair theory, which received support from several scientific groups. Positive holes (sites of electron deficiency) are activated in stressed rocks from pre-existing yet dormant positive hole pairs (PHPs) and their recombination at rock–air interface leads to a LST rise. A combination of remote sensing detection of rock mechanics behavior with a perception of chemistry and geophysics has been applied to propose the remote sensing rock mechanics theory. Remote sensing detections of such anomalies confirm so far proposed lab theories for such a hotly debated field as earthquake precursor study by providing unbiased observations with consistency in time and space distribution.