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991.
全国第二次土地调查是为了全面查清土地利用状况,掌握各类用地的分布和利用状况,以便相关部门掌握真实的土地基础数据,进而实现比较科学的宏观规划与管理。在土地调查的内业实践中分析了数据建库工作中容易出现的问题,在充分考虑建库数据的现势性和准确性的基础上提出了基于Arclnfo的控制建库数据质量的思路及具体方法。 相似文献
992.
在当前国家基础GIS数据分析的基础上,推出了利用GIS数据实现制作普通地理图、专题地图的技术路线,阐述了该技术路线的关键技术,并探讨了该技术路线的实用性。 相似文献
993.
城乡一体化空间数据库的建设是一个非常复杂的过程,它涉及到各个系统平台之间、各个部门之间、各种业务之间的协调和规划。参照国家的有关标准和规范建立一套地籍地形一体化编码体系、构造城乡一体化现代地籍系统平台的数据字典。只有符合标准编码规范和数据组织才能进入系统,才能被系统接纳。 相似文献
994.
995.
目前数字化测绘生产中大量数据主要依赖于硬盘存储,由于各种原因导致硬盘数据丢失时有发生。介绍了硬盘数据恢复的基本原理与方法,该方法能有效地恢复硬盘丢失的数据,确保数字化测绘生产数据的安全。 相似文献
996.
997.
针对现有房产测绘数据管理类软件无法很好的解决历史数据整理入库的问题,构建了一个具有图形数据与属性数据批量迁移功能的数据管理系统,实现了将数据批量入库进行统一管理的目的。本文对该系统的开发背景、设计原则、系统的主要功能和系统开发中一些实用的技术方案设计作了重点论述。 相似文献
998.
A large area hypoxia has been already reported respectively by two interdisciplinary surveys off the Changjiang Estuary since summer of 1999 and 2006. The hypoxic zone shows distinct year-to-year variations. Observed oceanographic data are first analysized and reveal a big difference for the Changjiang Diluted Water (CDW) between these two periods. These great changes are related to the tremendous reduction of the freshwater discharge and variations of wind fields between these two years. It is also found that the monthly mean intrusion of Kuroshio and its branches has increased in the northern East China Sea (ECS), but decreased in the southern ECS in August of 2006 as compared with 1999 on the base of general circulation models. Then, the Regional Ocean Modelling Systems is applied to the East China Sea to evaluate the contributions and relative importance of impacts from the river discharge, wind forcing and open boundary data. Our simulations reproduce the phenomena that more fresh water extends northeastward in 2006 and forms a negative SSS anomaly to the northeast of the river mouth as compared with 1999, which is consistent with observations. The five group numerical tests suggest that the wind forcing dominates the CDW variations followed by the Kuroshio and its branches. The study implies important roles played by hydrodynamic processes on the variability of hypoxic zone in the study areas. 相似文献
999.
Based on the comprehensive collection of the field observed salinity of the Bohai Sea (BHS) and the northern Huanghai Sea (NHS) from the 1950s to the present,the patterns of 10-years-averaged salinity at the different layers in the recent five decades (the 1950s,the 1960s,the 1970s,the 1980s and the 1990s) are obtained by the spatial-temporal interpolation technique with the scrupulous data quality control in this study.Then,by combining the spatial-temporal interpolation technique with successive correction method,the annual distributions of salinity both in the BHS and in the NHS are obtained as well.The data analyses indicate that the overall salinity in the BHS and the NHS increases from the 1960s till the present,with the increase of annual mean salinity of 0.04 psu from the 1950s,and the maximum increase rate of salinity is about 0.14 psu/a in the Bohai Bay.The high salinity tongue extended significantly from the NHS into the BHS.The intensified eastern wind field is related to the western intrusion of the NHS warm current,which probably leads to the moving forward of the high salinity water mass into the BHS.However,it is rather different from the salinity distribution characteristics between the 1950s and the 1960s.The extensive precipitation in the 1960s could lead to an increase in the discharge of the Huanghe River,which might result in the decrease of salinity in the BHS.But the salinity isoline of 32 in the NHS still extended significantly into the BHS in the 1960s.Since the 1980s,the patterns of salinity distribution have changed thoroughly.The salinity in the central area of the BHS was low,while the salinity in the Bohai Bay and the Liaodong Bay was higher than the other regions with its horizontal salinity gradient decreasing in the 1980s.The Empirical Orthogonal Function Analysis (EOF) is also conducted to study the interannual salinity variability of the BHS and the NHS.The correlation coefficient between the time coefficient series of the main mode and the Huanghe River discharge can reach -64.57%.It can be concluded that salinity variation of the BHS and the NHS has strong negative correlation with the Huanghe River discharge. 相似文献