Tropical Events: the Solstices and Equinoxes
☼ Tropical Events: the solstices and equinoxes This presentation is a simple layman‟s study of some interesting aspects of Earth‟s orbital history, especially concerning solstices and equinoxes, and the changing lengths of the days, seasons, and years. The charts below are from an Excel spreadsheet, created with an open source Excel Add-In, both of which I am making available at the end of this webpage: as I would have loved to have started out with something similar 10 years ago, when I first became interested in “the motions of the heavens” and the workings of the solar system. My first inquiry concerned the “mean tropical year”: why does it change? chart 21 mty.png days per mean tropical year in dynamical days of 86400 SI seconds days per mty 365.242750 365.242625 365.242500 365.242375 365.242250 365.242125 days 365.242000 365.241875 365.241750 365.241625 365.241500 0 80,000 20,000 40,000 60,000 -80,000 -60,000 -40,000 -20,000 100,000 -100,000 calendar year It is mostly due to the changing speed of the precession! The rate of precession is shown below in arcseconds per Julian year (365.25 days), a standard time increment used by astronomers. chart 2 rate of precession precess.png arcseconds per Julian year quasi-periodic approximation, Laskar et al 1993 degree 7 polynomials from data La93(0,1) Laskar 1986 (±10T) 53.00 52.75 52.50 52.25 52.00 51.75 51.50 51.25 51.00 50.75 50.50 50.25 50.00 arcseconds 49.75 49.50 49.25 49.00 48.75 48.50 48.25 48.00 0 20,000 40,000 60,000 80,000 -80,000 -60,000 -40,000 -20,000 100,000 -100,000 calendar
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