The New Zealand gravimetric quasigeoid model 2017 that incorporates nationwide airborne gravimetry

被引:14
作者
McCubbine, J. C. [1 ,4 ]
Amos, M. J. [2 ]
Tontini, F. C. [3 ]
Smith, E. [4 ]
Winefied, R. [2 ]
Stagpoole, V. [3 ]
Featherstone, W. E. [5 ]
机构
[1] Geosci Australia, Geodesy Sect, Community Safety & Earth Monitoring Div, GPO Box 378, Canberra, ACT 2601, Australia
[2] Land Informat New Zealand, POB 5501, Wellington 6145, New Zealand
[3] GNS Sci, 1 Fairway Dr, Lower Hutt 5011, New Zealand
[4] Victoria Univ Wellington, Wellington 6012, New Zealand
[5] Curtin Univ Technol, Inst Geosci Res, Dept Spatial Sci, GPOB U1987, Perth, WA 6845, Australia
关键词
Airborne gravity; Gravimetric quasigeoid; New Zealand; SLOPE VALIDATION SURVEY; GEOID DETERMINATION; GRAVITY; KERNEL; ACCURACY; HEIGHTS;
D O I
10.1007/s00190-017-1103-1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A one arc-minute resolution gravimetric quasigeoid model has been computed for New Zealand, covering the region - and -. It was calculated by Wong and Gore modified Stokes integration using the remove-compute-restore technique with the EIGEN-6C4 global gravity model as the reference field. The gridded gravity data used for the computation consisted of 40,677 land gravity observations, satellite altimetry-derived marine gravity anomalies, historical shipborne marine gravity observations and, importantly, approximately one million new airborne gravity observations. The airborne data were collected with the specific intention of reinforcing the shortcomings of the existing data in areas of rough topography inaccessible to land gravimetry and in coastal areas where shipborne gravimetry cannot be collected and altimeter-derived gravity anomalies are generally poor. The new quasigeoid has a nominal precision of on comparison with GPS-levelling data, which is approximately less than its predecessor NZGeoid09.
引用
收藏
页码:923 / 937
页数:15
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