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논문 기본 정보

자료유형
학술저널
저자정보
Jekeli, Christopher (Ohio State University) Yang Hyo Jin (Ohio State University) Kwon, Jay Hyoun (University of Seoul)
저널정보
한국측량학회 한국측량학회지 한국측량학회지 제31권 제6-2호
발행연도
2013.12
수록면
567 - 576 (10page)

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초록· 키워드

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The determination of the geoid in South Korea is a national imperative for the modernization of height datums, specifically the orthometric height and the dynamic height, that are used to monitor hydrological systems and environments with accuracy and easy revision, if necessary. The geometric heights above a reference ellipsoid, routinely obtained by GPS, lead immediately to vertical control with respect to the geoid for hydrological purposes if the geoid height above the ellipsoid is known accurately. The geoid height is determined from gravimetric data, traditionally ground data, but in recent times also from airborne data. This paper illustrates the basic concepts for combining these two types of data and gives a preliminary performance assessment of either set or their combination for the determination of the geoid in South Korea. It is shown that the most critical aspect of the combination is the gravitational effect of the topographic masses above the geoid, which, if not properly taken into account, introduces a significant bias of about 8 mgal in the gravity anomalies, and which can lead to geoid height bias errors of up to 10 cm. It is further confirmed and concluded that achieving better than 5 cm precision in geoid heights from gravimetry remains a challenge that can be surmounted only with the proper combination of terrestrial and airborne data, thus realizing higher data resolution over most of South Korea than currently available solely from the airborne data.

목차

Abstract
1. Introduction
2. Geoid Determination
3. Data Combination
4. Preliminary Data Analysis
5. Geoid Height Analyses
6. Conclusions
References

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