SUMMARY
The radius of the Earth has been determined through various methods over centuries, with significant contributions from ancient Greeks, notably Eratosthenes. Modern measurements utilize data from satellites, particularly the WGS-84 model, and techniques such as very long baseline interferometry. The International Earth Rotation Service provides detailed data sources for these models. Historical methods included astronomical observations and physical surveys, which were essential for refining mathematical models of the Earth's size and shape.
PREREQUISITES
- Understanding of WGS-84 Earth ellipsoid
- Familiarity with very long baseline interferometry
- Knowledge of satellite positioning systems
- Basic concepts of astronomical units and their historical context
NEXT STEPS
- Research the development and applications of the WGS-84 model
- Explore the principles of very long baseline interferometry
- Study the historical methods of measuring the Earth's size and shape
- Investigate the significance of the astronomical unit in planetary science
USEFUL FOR
Geographers, astronomers, physicists, and anyone interested in the historical and modern methods of determining the Earth's dimensions and shape.