Semi-kinematic geodetic reference frame based on the ITRF2014 for Malaysia

IF 0.9 Q4 REMOTE SENSING Journal of Geodetic Science Pub Date : 2020-01-01 DOI:10.1515/jogs-2020-0108
M. Azhari, Z. Altamimi, G. Azman, M. Kadir, W. Simons, R. Sohaime, M. Yunus, M. Irwan, C.A. Asyran, N. Soeb, A. Fahmi, A. Saiful
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引用次数: 3

Abstract

Abstract Malaysia is located at the stable part of the tec-tonic Sundaland platelet in SE Asia. The platelet is surrounded in almost every direction by tectonically active convergent boundaries, at which the Philippine Sea, the Australian and the Indian Plates are subducting respectively from the East, South and West.The current Malaysia geodetic reference frame called MGRF2000 is a static reference frame and hence did not incorporate the effects of plate motion and the ensuing deformation from (megath-rust) earthquakes. To prevent degradation of Continuously Operating Reference Station (CORS) coordinates, a new time-dependent national reference frame was developed. Taking advantage of the availability of the GNSS data of the CORS network in Malaysia, notably the Malaysia Active GPS System (MASS) and Malaysia Real-Time Kinematic GNSS Network (MyRTKnet), a more accurate and robust Malaysian geodetic reference frame was determined, fully aligned and compatible with ITRF2014. The cumulative solution obtained from stacking Malaysian CORS position time series formed the basis of the new MGRF2020 realization. It consists of 100+ station positions at epoch 2020.0, station velocities and Post-Seismic Deformation (PSD) parametric models for stations subjected to major earthquakes. The (1999-2018) position time series exhibit Weighted Mean Root Square (WRMS) values of 3.0, 3.2 and 7.6 mm in respectively the East, North and Vertical components. A new semi-kinematic geodetic datum (GDM2020) for Malaysia, useable for GIS, mapping and cadastre applications is proposed to replace the existing static datum (GDM2000). A transformation suite to convert the spatial databases from GDM2000 to GDM2020 was also developed.
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基于ITRF2014的马来西亚半运动学大地测量参考系
摘要马来西亚位于东南亚构造巽他陆板块的稳定部分。血小板几乎在每一个方向上都被构造活跃的收敛边界所包围,菲律宾海、澳大利亚板块和印度板块分别从东、南、西俯冲而下。目前的马来西亚大地测量参考系称为MGRF2000,是一个静态参考系,因此不包括板块运动和随后的地震变形的影响。为了防止连续运行参考站(CORS)坐标的退化,提出了一种新的时变国家参考系。利用马来西亚CORS网络的GNSS数据的可用性,特别是马来西亚主动GPS系统(MASS)和马来西亚实时动态GNSS网络(MyRTKnet),确定了一个更精确和强大的马来西亚大地测量参考框架,完全对齐并与ITRF2014兼容。通过叠加马来西亚CORS位置时间序列获得的累积解构成了新的MGRF2020实现的基础。它包括100多个台站在2020年历元的位置,台站速度和遭受大地震的台站的震后变形(PSD)参数模型。1999-2018年位置时间序列的加权均方根(WRMS)值分别为3.0、3.2和7.6 mm。马来西亚提出了一种新的半运动学大地测量基准(GDM2020),可用于GIS,地图和地籍应用,以取代现有的静态基准(GDM2000)。开发了GDM2000到GDM2020空间数据库转换套件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geodetic Science
Journal of Geodetic Science REMOTE SENSING-
CiteScore
1.90
自引率
7.70%
发文量
3
审稿时长
14 weeks
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