Kepler's Three Laws

Three observational rules that turned planetary motion into a closed-form science a century before Newton explained why.

Equal areas in equal times: shorter arc near perihelion sweeps the same area as the longer arc near aphelion.
Equal areas in equal times: shorter arc near perihelion sweeps the same area as the longer arc near aphelion.

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Kepler did not have calculus. He did not have Newton's gravity. He did not have a computer. He had twenty years of his boss Tycho Brahe's painstaking eyeballed-with-a-quadrant observations of Mars, and he had patience. Out of that he wrote three rules that are still exactly correct today, four hundred years later.

Law one: orbits are ellipses, not circles. Heretical at the time. Law two: the line from a planet to the Sun sweeps out equal areas in equal times — which is a sneaky way of saying planets speed up when they're close to the Sun and slow down when they're far. Law three: the bigger the orbit, the longer the year, in a precise way (T² scales as a³).

Newton came along seventy years later and proved that all three laws fall out of one simple gravity equation. But Kepler got there first, with no theory — just by staring at numbers until they confessed. That's the kind of move you can still pull in modern science if you have the patience for it.

Kepler's third law in modern form: T² depends only on a (and the central body's μ).

First law: planets orbit on ellipses with the Sun at one focus. Before Kepler, every model used circles — sometimes nested, sometimes offset, but always circular. Kepler used Tycho Brahe's twenty years of Mars observations and gave up: the data didn't fit circles, and nothing he could do made them. Ellipses fit on the first try.

Second law: the line from Sun to planet sweeps equal areas in equal times. This is angular-momentum conservation in disguise. Near perihelion the planet is close to the Sun, the line is short — so it has to swing fast to sweep the same area as a long, slow line near aphelion. It's why orbital speed isn't constant.

Third law: `T² ∝ a³`. The square of the orbital period is proportional to the cube of the semi-major axis. With Earth set to T = 1 year and a = 1 AU, you can read off any planet's period from its distance — or its distance from its period. Newton would later derive this from gravity; Kepler got there through pure pattern-matching on Brahe's data.

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