Discussion Overview
The discussion revolves around the concept of measuring sea level, particularly in relation to the Earth's shape, tidal influences, and various datums used for height measurements. Participants explore how sea level is defined and measured across different regions, considering factors such as the Earth's ellipsoidal shape and local variations in sea level.
Discussion Character
- Exploratory
- Technical explanation
- Debate/contested
- Mathematical reasoning
Main Points Raised
- Some participants inquire about the existence of a median sea level used for data logs, emphasizing the need for a reference based on distance from the Earth's center.
- Others note that different countries have their own mean sea levels and that the geoid used for GPS is not necessarily aligned with actual sea levels.
- A participant mentions the historical use of various datums, including a 1927 USGS datum and a 1989 average sea level datum, highlighting inconsistencies in local applications.
- There is a discussion about the polar radius being the lowest point on Earth and whether world sea level could be approximated to this level, excluding tidal effects.
- Some participants argue that local sea level can vary significantly due to geological factors, such as crustal deformation and variations in local gravity.
- One participant raises a question about ocean currents and their potential effects on sea level uniformity, suggesting that water's viscosity might influence how sea levels propagate.
- A mathematical formulation for geocentric latitude and Earth's radius is provided, indicating a technical approach to understanding the Earth's shape and its implications for sea level measurement.
Areas of Agreement / Disagreement
Participants express multiple competing views regarding the definition and measurement of sea level, with no consensus reached on a singular approach or understanding. The discussion remains unresolved, particularly around the implications of the Earth's shape and local variations.
Contextual Notes
Limitations include the dependence on various historical datums, the complexity of local geological factors affecting sea level, and the lack of a universally accepted mean sea level reference across different regions.