Astronomy & Celestial Mechanics
the sky, computed
Series

Phases and eclipses — the series

3 essays on one idea, from the one that introduces it to the one that assumes the rest.
  1. Phases are a viewing angle, not a shadow. A satellite at eight points of its orbit. Exactly half of it is lit at every one of them; what changes is how much of the lit half faces the centre. Nothing is in shadow except at an eclipse.

    Phases are not shadows, and eclipses are

    Half the Moon is lit at every instant of every month. The phase is which part of the lit half faces the Earth — and confusing that with a shadow is the commonest error in astronomy.

    part 1 · sky
  2. Three periods that nearly share a multiple. How far the draconic and anomalistic months are from a whole number, after a whole number of synodic months, in hours. At 223 synodic months — 6585.321 days — both are within an hour of closing, which is what makes an eclipse repeat. The draconic residual is 0.87 hours and the anomalistic 5.19 hours.

    The eclipse that repeats a third of a world away

    Three lunar periods nearly share a multiple after 6,585 days. The word "nearly" is what makes eclipses predictable, and the leftover third of a day is what moves each repeat a third of the way round the Earth.

    part 2 · sky
  3. A limb 6.2 kilometres from its highest point to its lowest. The Moon's edge, drawn as the height of the local horizon above a mean circle, against position angle around the limb. The profile has an root-mean-square amplitude of 1.2 kilometres and reaches 3.1 at its extremes, which at the Moon's distance is 3.35 arcseconds — against a solar radius of 960. The valleys marked are the places where sunlight survives longest at second contact and reappears first at third, which is what produces Baily's beads. Every eclipse timing is a measurement of when a particular point of this profile crossed the solar limb, so extracting a solar diameter from a contact time requires the profile at the libration of that day, to a precision of a few hundred metres.

    A solar radius measured past a mountain range

    The most accurate way to measure the Sun's diameter is to time an eclipse. What is timed is the moment sunlight vanishes behind the Moon's edge — and the Moon's edge is a horizon with mountains on it, so the measurement is a difference between the Sun's limb and a lunar landscape that has to be supplied from somewhere else.

    part 3 · sky

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