• Title/Summary/Keyword: EIGEN-CG01C

Search Result 2, Processing Time 0.015 seconds

Accuracy Analysis of New Geopotential Model using GPS/Levelling Data (GPS/Levelling데이터를 사용한 새로운 지구중력장모델의 정확도 분석)

  • Yun Hong-Sic;Cho Jae-Myoung
    • Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
    • /
    • v.23 no.4
    • /
    • pp.353-358
    • /
    • 2005
  • The purpose of this paper is to evaluate a new geopotential model, EIGEN-CG01C which had been developed from CHAMP and GRACE mission observations and surface gravity data. The accuracy analysis was conducted by comparing the geoidal heights computed from two types of geopotential models (i.e., EIGEN-CG01C and EGM96) with spirit leveled GPS bench mark. To this end, three hundred twenty GPS leveled bench marks are used as bases for the numerical investigation. From the analysis, it was possible to conclude that EIGEN-CG01C was more suitable to upgrade the KGEOID 98 since the results that the EGM96 was slightly biased.

Gravity Potential Comparative Analysis around Korean Peninsula by EGM96 and EIGEN-CG01C Models (EGM96와 EIGEN-CG01C 모델에 의한 한반도 주변의 중력포텐셜 비교분석)

  • Yu, Sang-Hoon;Kim, Chang-Hwan;Min, Kyung-Duck
    • 한국지구물리탐사학회:학술대회논문집
    • /
    • 2005.05a
    • /
    • pp.261-266
    • /
    • 2005
  • According to development of satellite geodesy, gravity potential models which have high accuracy and resolution were released. Using the EIGEN-CG01C model based on low orbit satellite data such as CHAMP and GRACE and the EGM96 model, geoid and gravity anomaly were calculated and compared. The study area is located at $123^{\circ}{\sim}132^{\circ}$ E, $33^{\circ}{\sim}43^{\circ}$ including Korea. Comparing two models, very high correlation more than 0.90 in geoid and gravity anomaly was observed, but in amplitude analysis the EIGEN-CG01C model have higher amplitude in high frequency area. Gravity anomaly calculated with both models shows a little difference in North Korea and some coast area of the Yellow sea. Through power spectrum analysis, residual anomaly that can be used in large scale structure or underground resources survey was calculated.

  • PDF