利用InSAR-GIS监测西安地面沉降的分析研究

针对合成孔径雷达干涉测量（InSAR）技术在监测地表形变的数据后处理及成果表达和分析方面存在的一些局限性问题,研究通过GIS数据库管理InSAR监测数据和相关区域的地理、水准及GPS数据等辅助数据,以及利用GIS空间分析功能埘监测结果进行分析的方法与实现。以西安地区InSAR数据为研究对象对提出的方法进行实现,试验结果表明,GIS技术与InSAR技术卡“结合用于地面沉降监测可以有效地解决在监测地表形变的数据后处理及成果表达和分析方面的局限性问题。     

Research on Autonomous Orbit Determination of Navigation Satellite Based on Crosslink Range and Orientation Parameters Constraining

Introduction Thepotentialvulnerabilityofsatellitenaviga tionsystemthatreliesongroundstationsisthat thesystemwouldbreakdownifgroundstations weredestroyed,whichcannotmeettherequire mentofnavigationwarfare[1].Withthedevelop mentofsuchspace basedsystemsasgrou…     

时序InSAR多源数据地面沉降监测研究

随着遥感技术的发展,基于时间序列的合成孔径雷达干涉测量(时序InSAR)技术凭借全天时不接触、不易受环境影响、监测效率高等优势,极其适用于对大面积地面进行微小形变应用.通过对时序InSAR多源数据的研究,选取合理的数据源和数据处理方法进一步提高监测精度.     

Study on Recovering the Earth＇s Potential Field Based on GOCE Gradiometry

Given the second radial derivative Vrr（P） ｜δs of the Earth＇s gravitational potential V（P） on the surface δS corresponding to the satellite altitude, by using the fictitious compress recovery method, a fictitious regular harmonic field rrVrr（P）^＊ and a fictitious second radial gradient field V：（P） in the domain outside an inner sphere Ki can be determined, which coincides with the real field V（P） in the domain outside the Earth. Vrr^＊（P）could be further expressed as a uniformly convergent expansion series in the domain outside the inner sphere, because rrV（P）^＊ could be expressed as a uniformly convergent spherical harmonic expansion series due to its regularity and harmony in that domain. In another aspect, the fictitious field V^＊（P） defined in the domain outside the inner sphere, which coincides with the real field V（P） in the domain outside the Earth, could be also expressed as a spherical harmonic expansion series. Then, the harmonic coefficients contained in the series expressing V^＊（P） can be determined, and consequently the real field V（P） is recovered. Preliminary simulation calculations show that the second radial gradient field Vrr（P） could be recovered based only on the second radial derivative V（P）｜δs given on the satellite boundary. Concerning the final recovery of the potential field V（P） based only on the boundary value Vrr （P）｜δs, the simulation tests are still in process.     

A Research on the Monitoring of Coastal Land use with Aerial Photographs in the Example of Kadırga bay (Çanakkale)

In coastal areas, environmental monitoring is an important tool in acquiring data to achieve the goal of sustainable usage relating to the character of changes in quantity and quality of land cover / land use. Studies can reveal the diversity of species and the natural factors and human influence affecting this diversity, occurring as a result of habitat fragmentation or destruction. As well as comparing the past and current state of environmental resources, monitoring helps to determine trends in the use and changes of resources. It was in this context that Kad?rga Bay, located on the northwest coast of Canakkale province, Turkey was studied. Also situated in this location is Assos, a significant site in ancient history with great tourism potential. This study determined changes in land cover / land use by means of photogrammetrical interpretation of data from 1957 to 2002. The research further aimed to determine pressure on the components of the ecological structure of the area. Based on the data obtained, projections can be made to protect the future, and will provide an important source for management of the area. Within the 45-year study period, it was determined that agriculture and secondary housing construction exerted the most pressure on the habitat of the area. In the main, an increase in agricultural activities and secondary house construction emerged as the cause of a decrease in wetlands and forest areas.     

Estimation of the Resolution of Earth＇s Gravity Field for GRACE Follow-On Using the Spectrum Method

利用轨道扰动引力谱和大地水准面累计误差谱分析的方法估计未来GRACE（gravity recovery and climate experimenl）Follow—On卫星反演地球重力场的空间分辨率。基于GRACEFollow—On卫星的轨道特性,计算其在高空所受到的径向扰动引力,并根据谱特性及星载加速度计的测量噪声水平分析该卫星能反演重力场的阶数。利用EGM96重力场模型分别计算200km和250km轨道高度处的扰动引力谱。分析其特性表明：在两个轨道高度处分别能反演281阶和242阶的地球重力场模型。给出大地水准面累计误差谱模型,并计算200km和250km轨道高度处大地水准面累计误差谱。分析其谱特性表明：在两个轨道高度处分别能反演至286阶和228阶的地球重力场模型。     

A Fitting Algorithm of the Apparent Moon Center and Its＇ Application on Fast Orientation

基于电子经纬仪对月球明亮区域边沿的观测采样,提出一种月球视圆面中心拟合算法,推导出详细的计算公式。通过实际观测试验验证该算法的可靠性,较好地解决了月面中心的确定问题。在此基础上,探索一种测月快速定向方法。运用此方法进行天文定向,内符合精度和外符合精度均优于±2．0”。测月定向可有效弥补传统天文定向夜间只能依靠观测恒星进行的不足,扩展天文测量的使用范围。由于太阳的视面也是正圆,测月定向方法同样适用于测日定向。