| 英文摘要 |
Geodetic Datum serves as the fundamental spatial reference framework for national surveying, mapping, and geospatial information applications. During the era when triangulation was the primary surveying technique, the global connection of geodetic datums was mainly achieved through astronomical observations. With advances in geodetic technology, the integration of space geodetic technologies, such as Very-Long Baseline Interferometry (VLBI), Satellite Laser Ranging (SLR), and Global Navigation Satellite Systems (GNSS), has established a solid foundation for the realization of a globally unified and highly accurate spatial reference framework. At present, most countries have adopted national geodetic datums based on networks of GNSS Continuous Operating Reference Stations (CORS), and aligned with the International Terrestrial Reference Frame (ITRF) at a specific reference epoch. Taiwan’s geodetic datum, TWD97, is also implemented under this framework. As tectonic plate motion, crustal deformation, and seismic activities have become increasingly significant, geodetic datums have gradually evolved from static models toward dynamic frameworks capable of reflecting temporal variations. In 1998, New Zealand officially released and implemented a semi-dynamic geodetic datum known as the New Zealand Geodetic Datum 2000 (NZGD2000), marking an important milestone in this transition, representing a new stage in national geodetic datum management that considers both spatial and temporal changes.. This paper reviews the geodetic datum developments in the United States, Japan, the European Union, Australia, and New Zealand, and analyzes the approaches to reference frame maintenance, epoch updates, and dynamic management. The findings are intended to provide important references for the planning and development of the next-generation geodetic datum in Taiwan. |