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昆明冶金高等专科学校学报 ›› 2025, Vol. 41 ›› Issue (05): 19-.DOI: 10.3969/j.issn.1009-0479.2025.05.004

• 资源开发与测绘 • 上一篇    下一篇

利用高程异常控制点对重力场模型的纠正研究

  

  1. 1.昆明冶金高等专科学校测绘学院,云南 昆明 650033;2.云南省测绘产品检测站,云南 昆明 650034; 3.昆明市测绘研究院,云南 昆明 65023
  • 出版日期:2025-10-01 发布日期:2026-03-25
  • 作者简介:陈 占 (1985-),男,河南商丘人,讲师,工学硕士,无人机应用技术技能大师工作室成员,主要从事测绘科学与技术方面教学与研究工作。

Research on Correction of Gravity Field Models UsingElevation Anomaly Control Points

  1. 1. Faculty of Surveying and Mapping, Kunming metallurgy College, Kunming 650033, China;
    2. Yunnan Test Station of Mapping and Surveying Products, Kunming 650034, China;3. Kunming Instijute of Surveying and Mapping, Kunming 650233, China
  • Online:2025-10-01 Published:2026-03-25

摘要: 采用传统测量方法获取控制点高程的方式,精度高但耗时费力。如何快速获取高精度的正常高是近来 测绘领域研究的课题之一。提出了一种顾及 EGM2008和 SGGUGM2两个全球重力场模型的 GNSS高程拟合方 法。首先利用重力场模型生成重力似大地水准面,再根据实测数据与重力场模型生成差值曲面。最后将差值曲 面与重力似大地水准面进行融合,从而将重力似大地水准面拟合适配于似大地水准面,实现利用高程异常控制 点对重力场模型的纠正的目的。文中利用 EGM2008和 SGGUGM2两个重力场模型,借助云南省似大地水准面 精化模型进行精度检测,根据检测结果显示,该方法稳定可靠,能满足常见的大比例尺地形图测绘等应用。

关键词: 高程异常, 重力场模型, 似大地水准面, EGM2008重力模型, SGGUGM2重力模型

Abstract: Traditional measurement methods for obtaining the elevation of control points are high accuracybut time-consuming and labor-intensive. How to quickly acquire high-precision normal height has be-come one of the recent research topics in the field of surveying and mapping. This article proposes aGNSS elevation filtting method that considers two global gravity field models, namely EGM2008 and SGG-UGM-2. First, the gravity field model is used to generate gravity quasi-geoid; then a difference surface isgenerated based on the measured data and the gravity field model. Finally, the difference surface is fusedwith the gravity quasi-geoid to fit the gravity quasi-geoid to the actual quasi-geoid, thereby achieving thepurpose of correcting the gravity field models using the elevation anomaly points. In this paper, theEGM2008 and SGG-UGM-2 gravity field models are used, and the refined quasi-geoid model of YunnanProvince is adopted for accuracy verification. The test results, show that this method is stable and relia-ble, and can meet the requirements of common applications such as large-scale topographic mapping.

Key words: elevation anomaly, gravity feld models:Quas1-Geo1d:
EGM2008 Gravity Model:SGGUGM-2 Gravity Model