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Historical eclipses and the earth's rotation
1Department of Physics, University of Durham, UK.
Science Progress
|May 9, 2000
Summary
Ancient eclipse records reveal long-term changes in Earth's rotation. Analysis shows the day is lengthening by 1.7 milliseconds per century, less than tidal predictions.
Area of Science:
- Geophysics
- Astronomy
- Earth Sciences
Background:
- Historical eclipse records provide valuable long-term data for geophysics.
- Ancient observations, though seemingly crude, allow investigation of Earth's rotation variations over millennia.
- Limited reliable historical records originate from Babylonian, Chinese, European, and Arab cultures.
Purpose of the Study:
- To analyze ancient eclipse observations for insights into Earth's rotation.
- To investigate long-term trends in the length of the day.
- To compare historical data with modern geophysical models, particularly tidal effects.
Main Methods:
- Compilation and analysis of historical records of solar and lunar eclipses.
- Categorization of observations into precise timings and qualitative descriptions.
- Comparison of ancient data with tidal friction models.
Main Results:
- Ancient eclipse data reveals long-term trends in the length of the day.
- The average rate of day lengthening over 2,500 years is 1.7 milliseconds per century.
- This rate is significantly less than the 2.3 milliseconds per century predicted by tidal friction.
Conclusions:
- Ancient eclipse observations are crucial for understanding long-term changes in Earth's rotation.
- Historical data provides a unique, long-term perspective unobtainable from modern telescopic observations.
- Discrepancies between historical data and tidal models suggest other mechanisms influence Earth's rotation rate.