Abstract

An eclipse on 188 BC July 17 was observed and recorded both at Chang’an (China) and Rome (Italy). An eclipse on AD 873 July 28 was observed and recorded both at Nishapur (Iran) and Kyoto (Japan). The eclipse was annular at Nishapur. These plural records of deep eclipses are rare in history, and are useful for determining the clock correction, $\Delta T$, and the lunar tidal acceleration, $\dot{n}$. We have tried to determine as precisely as possible the ranges of these two parameters. If we fix the tidal acceleration to $- {25\rlap {.}{}^{\mathrm {\prime \prime }}83} \,\mathrm{cy}^{-2}$, we get, as a best estimate, $12581 \,\mathrm{s} < \Delta T < 12741 \,\mathrm{s}$ from the 188 BC eclipse and contemporary eclipses, and $3327 \,\mathrm{s} < \Delta T < 3498 \,\mathrm{s}$ from the AD 873 eclipse and contemporary eclipses.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.