Airborne geoid mapping of land and sea areas of East Malaysia

This paper describes the development of a new geoid-based vertical datum from airborne gravity data, by the Department of Survey and Mapping Malaysia, on land and in the South China Sea out of the coast of East Malaysia region, covering an area of about 610,000 square kilometres. More than 107,000 k...

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Bibliographic Details
Published in:Journal of Geodetic Science (Online) 2017-02, Vol.7 (1), p.84-93
Main Authors: Jamil, H., Kadir, M., Forsberg, R., Olesen, A., Isa, M. N., Rasidi, S., Mohamed, A., Chihat, Z., Nielsen, E., Majid, F., Talib, K., Aman, S.
Format: Article
Language:English
Subjects:
Airborne gravimetry
East Malaysia
geoid modelling
seamless vertical datum
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Summary:This paper describes the development of a new geoid-based vertical datum from airborne gravity data, by the Department of Survey and Mapping Malaysia, on land and in the South China Sea out of the coast of East Malaysia region, covering an area of about 610,000 square kilometres. More than 107,000 km flight line of airborne gravity data over land and marine areas of East Malaysia has been combined to provide a seamless land-to-sea gravity field coverage; with an estimated accuracy of better than 2.0 mGal. The iMAR-IMU processed gravity anomaly data has been used during a 2014-2016 airborne survey to extend a composite gravity solution across a number of minor gaps on selected lines, using a draping technique. The geoid computations were all done with the GRAVSOFT suite of programs from DTU-Space. EGM2008 augmented with GOCE spherical harmonic model has been used to spherical harmonic degree N = 720. The gravimetric geoid first was tied at one tide-gauge (in Kota Kinabalu, KK2019) to produce a fitted geoid, my_geoid2017_fit_kk. The fitted geoid was offset from the gravimetric geoid by +0.852 m, based on the comparison at the tide-gauge benchmark KK2019. Consequently, orthometric height at the six other tide gauge stations was computed from H = h - N . Comparison of the conventional (H ) and GPS-levelling heights (H ) at the six tide gauge locations indicate RMS height difference of 2.6 cm. The final gravimetric geoidwas fitted to the seven tide gauge stations and is known as my_geoid2017_fit_east. The accuracy of the gravimetric geoid is estimated to be better than 5 cm across most of East Malaysia land and marine areas
ISSN:2081-9943
2081-9943
DOI:10.1515/jogs-2017-0010