1984年世界大地测量系统-通过发展新的地球势模式EGM96而增强的总结

P. Fell
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引用次数: 1

摘要

仅给出摘要形式,内容大致如下。EGM96是一个由360度、360阶的球谐系数组成的地球位势模型。该模型是美国国家图像和测绘局、美国宇航局戈达德太空飞行中心和俄亥俄州立大学合作的结果,由海军水面作战中心提供支持。该联合项目利用了来自全球许多不同地区的新地表重力数据,包括NIMA档案新发布的数据。自1990年以来,NIMA主要的地面重力采集包括由海军研究实验室对格陵兰岛和北极和南极部分地区进行的空中重力测量,以及与利兹大学合作的重力收集项目。这些收集工作改善了世界上许多陆地地区的数据储备,包括非洲、加拿大、南美洲和非洲的部分地区、东南亚、东欧和前苏联。EGM96还包括来自美国海军GEOSAT大地测量任务和ERS-1在北极和南极部分地区的高度计得出的异常,以及威德尔海的高度计得出的异常。其他有助于EGM96的数据包括来自TOPEX/POSEIDON、ERS-1和GEOSAT的直接卫星测高数据,以及使用卫星激光测距(SLR)、全球定位系统、DORIS、跟踪和数据中继卫星系统以及TRANET对20多颗卫星的卫星跟踪。此外,为了减少原始地表重力数据,并准备30'/spl次/30'重力异常,从所有可用资源中组装了一个新的地形数据库。这个数据库还被用来计算地球上大约3%的地表重力数据不可用的均衡值。这个新的地势模型被用作更新WGS 84的大地测量参考。此外,它还将作为精确轨道、海洋学和地球物理研究的先进模型。本文将总结EGM96的开发成果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
World geodetic system 1984-a summary of enhancements through the development of the new geopotential model EGM96
Summary form only given, substantially as follows. EGM96 is a geopotential model of the Earth consisting of spherical harmonic coefficients complete to degree and order 360. This model is the result of a collaboration between the National Imagery and Mapping Agency, the NASA Goddard Space Flight Center and the Ohio State University, supported by the Naval Surface Warfare Center. The joint project took advantage of new surface gravity data from many different regions of the globe, including data newly released from the NIMA archives. Major terrestrial gravity acquisitions by NIMA since 1990 include airborne gravity surveys over Greenland and parts of the Arctic and the Antarctic, surveyed by the Naval Research Laboratory, and cooperative gravity collection projects, several which were undertaken with the University of Leeds. These collection efforts improved data holdings over many of the world's land areas, including Africa, Canada, parts of South America and Africa, Southeast Asia, Eastern Europe, and the former Soviet Union. EGM96 also included altimeter derived anomalies derived from the U.S. Navy's GEOSAT geodetic mission and from ERS-1 over portions of the Arctic and Antarctic, as well as the altimeter derived anomalies over the Weddell Sea. Other data that contributed to EGM96 were direct satellite altimetry from TOPEX/POSEIDON, ERS-1 and GEOSAT, and satellite tracking to over 20 satellites using satellite laser ranging (SLR), the Global Positioning System, DORIS, Tracking and Data Relay Satellite System, and TRANET. In addition, a new topographic data base was assembled from all available sources in order to reduce raw surface gravity data and prepare the 30'/spl times/30' gravity anomalies. This database was also used to calculate isostatic values in the roughly 3 percent of the globe where surface gravity data was not available. This new geopotential model is being used as a geodetic reference to update WGS 84. In addition, it will serve as a state of the art model for precise orbit, oceanographic, and geophysical studies. The paper will summarize the results of the EGM96 development.
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