7. Ptolemy, Copernicus, Tycho Brahe, and Kepler

A. Aristarchus and others measure the distance to the Moon

The ancient Greeks gave several reasons for believing that the Earth was a sphere. One of the most convincing was based on lunar eclipses. They realized that in a lunar eclipse, the Earth's shadow was projected on the Moon. The edge of this shadow was always circular, regardless of the relative positions of the Earth and the Moon. This could only be the case if the Earth were a sphere (a disk would cast a narrow elliptical shadow in some orientations).

Aristarchus (c. 250 B.C.) realized that lunar eclipses could be used for estimating the distance to the Moon in terms of the diameter of the Earth. Although his value was too low by about a factor of 3, later Greek astronomers, using his method, got very nearly the correct answer of about 30 Earth diameters. The steps in this calculation are as follows:

B. The motion of the planets on the celestial sphere.

C. The Ptolemaic system

D. The Copernican system

E. Tycho Brahe: precision observing without a telescope

F. Kepler: How the Planets Move (Part 1)

a. Tycho's excellent judgement

b. Kepler's first law

The orbits of the planets around the Sun are ellipses, with the Sun at one focus.

G. Overview

End lecture 7 2/4/03

Lecture 8: Kepler: How the planets move (Part 2); Galileo's experiments in dynamics

Course Plan

Home Page


Last updated 4 February 2003

Alan Stockton (stockton@ifa.hawaii.edu)