基于速度场模型的区域CGCS2000坐标实时转换

从WGS84到CGCS2000的坐标转换,涉及坐标框架转换和历元转换两个问题。如何提高大区域坐标转换精度,是一直以来的研究热点,针对大区域坐标转换精度较低的问题,考虑历元转换,提出融合速度场改正信息的坐标转换方法。该方法对建立速度场改正模型进行了研究,分析比较了各模型的精度和可靠性,在此基础上选择一种模型用于实现CGCS2000坐标实时转换。实例表明,该转换方法不受区域范围的影响,精度高且误差在各方向上都分布均匀。     

CGCS2000高精度坐标转换格网模型的建立

CGCS2000启用后,用于地形图图廓线和坐标网变换的高精度坐标转换格网模型的建立成为实用中的重要问题。本文阐述我国CGCS2000高精度坐标转换格网模型的建立方法。一是讨论坐标转换最小曲率方程,该方程同时具备整体光滑和局部光滑特性,可以更好地符合地图线状要素坐标转换时的连续光滑性;二是提出格网节点迭代计算方法以及拟合推估两步极小法构建区域性格网模型的方法,构建了格网模型数据结构;三是给出全国范围CGCS2000高精度坐标转换格网模型的最优格网间距和转换精度,按48 433个2000国家大地控制网点坐标构建了BJS54和XAS80到CGCS2000坐标转换格网模型,转换后的点位外符精度分别为0.26m和0.03m。     

基于CGCS 2000的高斯平面坐标与城市独立平面坐标转换的研究

在假设一种已知重合点坐标无误差情况下,推导了平面四参数坐标转换模型与平面六参数坐标转换模型的公式,该算法无需由误差方程组成法方程。同时,结合城市独立平面坐标与CGCS 2000平面坐标转换算例进行验证,得出了一些有益结论。     

GAMIT/GLOBK坐标系到CGCS2000坐标系的转换研究

由于CGCS2000坐标系的推广与应用,GAMIT/GLOBK解算坐标也需转换到CGCS2000系,在分析两者关系的基础上,根据IERS提供的框架间转换参数,通过坐标转换的方式进行归化。经过实验分析,结果表明采用这种方式可以得到精度优于2 cm的CGCS2000坐标,能够满足实际工程的需要。     

WGS-84(G1674)与CGCS2000坐标转换研究

简要介绍了WGS-84(G1674)与2000国家大地坐标系(CGCS2000)的背景,说明两者之间进行坐标转换的必要性,举例说明了坐标转换模型及可行的模型参数求解策略,最后评定了可达到的转换精度。     

CGCS2000与独立坐标系转换模型适用性研究

针对CGCS2000与城市独立坐标系转换中,如何根据需要选择合适转换模型,使产生的转换坐标具有高精度或者高符合性问题,利用CGCS2000与独立坐标系边长差和方位角差比较方法,分析转换模型特性。并通过实例对常用转换模型进行验证,归纳出模型的适用性,解决坐标转换中不同需求模型选择问题。文中方法对其它坐标转换有一定借鉴作用。     

ITRF2000框架坐标转换到ITRF1997框架下的研究与应用

在随着2000国家大地坐标系在全国不断推广与应用,将ITRF2000框架下的坐标转换到CGCS2000框架时,需先转换到ITRF1997框架下。本文采用布尔沙-沃尔夫模型对基于不同基准的两框架之间进行坐标转换,设计了七参数求解程序,并通过实例分析验证其准确性和可靠性。     

东莞市2000国家大地坐标系转换的思路与探讨

本文根据国家及省的相关工作要求及技术规范,结合地方城市特点,提出了东莞市坐标到2000国家大地坐标系(简称CGCS2000)转换的思路和技术路线,介绍了转换参数模型的建立与校验方法,通过转换模型软件开发,完成全市基础地理信息数据的转换工作。     

浅析宁波市2000国家大地坐标联测

宁波市2000国家大地坐标联测,获取了宁波市2000国家大地坐标系的大地基准和原有GPS控制点的2000国家大地坐标成果,并经过实地检测验证;更新了宁波市GPS控制点的54坐标系、80坐标系的平面坐标,建立了已有坐标系与2000国家大地坐标系的坐标转换关系,实现了基于NBCORS网络RTK技术的似大地水准面成果联合应用。     

浅析宁波市2000国家大地坐标联测

宁波市2000国家大地坐标联测,获取了宁波市2000国家大地坐标系的大地基准和原有GPS控制点的2000国家大地坐标成果并经过实地检测验证,更新了宁波市GPS控制点的54坐标系、80坐标系的平面坐标,建立了已有坐标系与2000国家大地坐标系的坐标转换关系,实现了基于NBCORS网络RTK技术的似大地水准面成果联合应用。     

WRC-2000

The forthcoming World Radiocommunication Conference (WRC) will deal with frequency allocation and protection issues that are of fundamental importance to GNSS (Global Navigation Satellite System) and GPS (Global Positioning System), which is a component of GNSS. In many countries, GPS L1 and L2 are not protected, and much needs to be done to obtain a frequency allocation for GPS L5. A brief explanation of the International Telecommunication Union (ITU) and how it can impact satellite navigation at its World Radiocommunication Conference in 2000 (WRC-2000) is provided. ? 2000 John Wiley & Sons, Inc.     

World Geodetic Datum 2000

 Based on the current best estimates of fundamental geodetic parameters {W ₀,GM,J ₂,Ω} the form parameters of a Somigliana-Pizzetti level ellipsoid, namely the semi-major axis a and semi-minor axis b (or equivalently the linear eccentricity ) are computed and proposed as a new World Geodetic Datum 2000. There are six parameters namely the four fundamental geodetic parameters {W ₀,GM,J ₂,Ω} and the two form parameters {a,b} or {a,ɛ}, which determine the ellipsoidal reference gravity field of Somigliana-Pizzetti type constraint to two nonlinear condition equations. Their iterative solution leads to best estimates a=(6 378 136.572±0.053)m, b=(6 356 751.920 ± 0.052)m, ɛ=(521 853.580±0.013)m for the tide-free geoide of reference and a=(6 378 136.602±0.053)m, b=(6 356 751.860±0.052)m, ɛ=(521 854.674 ± 0.015)m for the zero-frequency tide geoid of reference. The best estimates of the form parameters of a Somigliana-Pizzetti level ellipsoid, {a,b}, differ significantly by −0.39 m, −0.454 m, respectively, from the data of the Geodetic Reference System 1980. Received: 1 February 1999 / Accepted: 31 August 1999     

CGCS2000板块模型构建

基于中国地壳运动观测网络2001—2010年跨度长达10年的观测数据,采用基准优选、变异点数据分段处理等策略,计算获得ITRF2005框架下高精度速度场。同时针对国际上现有的NNR NUVEL1A、APKIM2005、PB2002等板块模型在中国区域适应性差,基于中国地质构造特性及实际速度场解算结果,构建了中国20个二级板块模型CPM-CGCS2000。采用本文提出的用板块模型参数将站点归算至CGCS2000的方法对板块模型进行外部检核,并用此方法验证所建的二级块体模型,精度可达2～3 cm。与国际上现有比较成熟的速度场模型———ITRF2005、APKIM2005、PB2002、NUVEL1A及国内文献[1—2]的板块模型进行的比较表明,CPM-CGCS2000板块模型实际精度优于目前现有的模型。     

Reflections on Mapping Census 2000

Mapping Census 2000: The Geography of U.S. Diversity is an atlas containing 75 maps and presenting county- and state-level data for Census 2000. Cynthia Brewer and Trudy Suchan rapidly produced the atlas in the Population Division of the U.S. Census Bureau using ArcInfo 8.1 prerelease software. Redistricting data, on which the atlas was based, were released in March 2001 and the full-color atlas went to press in July 2001. It is the first decennial atlas produced by the Census Bureau in 80 years. Race maps in the atlas are designed to present the new Census 2000 data that include counts of people who indicated more than one race. Choropleth classifications are constructed to facilitate comparison among maps in series for all race/ethnicity groups, both large and small. Map series share breaks that are adjusted to include meaningful breaks based on overall U.S. percentages for individual groups. Additional shared meaningful breaks, such as "no change" and "50 percent of the population" also anchor classifications. Maps of prevalent groups and diversity provide syntheses of race/ethnicity data. Maps were evaluated at numerous levels in the Census Bureau, with issues from topic selection to page layout to title wording debated by many people. The essay describes the production processes, agency standards, and cartographic principles that come together to present these new data in an atlas that is a colorful showpiece.     

CGCS2000框架维持方法分析

针对目前国内各GNSS应用在归算到2000国家大地坐标系（CGCS2000）时常采用强制符合及拟稳平差方法存在的问题及局限性,利用国家测绘地理信息局收集的全国近1 800个连续运行参考站（Continuously Operating Reference Stations,CORS）连续观测1个月的数据进行数据处理得到的基线解,分别基于强基准拟稳平差方式及顾及板块运动的速度场归算方法获得测站在CGCS2000下的坐标,分析两者的差异及误差分布情况,指出对于省级CORS站纳入CGCS2000的情况,采用强制符合拟稳平差方法所基于的基准站必须考虑板块的运动趋势进行CGCS2000归算,否则平差结果与CGCS2000最大差异将达到dm量级。     

ITRF2000参考架的评价及其探讨

通过ITRF2 0 0 0速度场建立完全独立于任何地质模型假设的ITRF2 0 0 0VEL模型 ,求出总角动量 |L|为 0 .12 7°/m·a ,在运动中应加以改正 ,从而实现无整体旋转参考架     

GIS能平安度过2000年吗

本文论述了2000年的问题对GIS产业发展的不利影响,分析了它所产生的根源,阐述了解决这一问题的方案。     

Comparative assessment of CORINE2000 and GLC2000: Spatial analysis of land cover data for Europe

Given the current lack of interoperability between global and regional land cover products, efforts are underway to link the new European global land cover map (GLOBCOVER) with the existing global land cover 2000 map (GLC2000) and European CORINE mapping initiative. Since both datasets apply different mapping standards, key for a successful implementation is a thorough understanding of the heterogeneities among both datasets. Thus, this paper provides an assessment of compatibilities and differences between the CORINE2000 and GLC2000 datasets. The comparative assessment considers inconsistencies between the thematic legends (using the UN land cover classification system-LCCS), class specific accuracies, and the spatial resolution and heterogeneity of the datasets. The results are summarized with implications for the development of the new GLOBCOVER datasets.