ch 2.2 readings
Learning Objectives
By the end of this section, you will be able to:
Describe early examples of astronomy around the world.
Explain how Greek astronomers deduced that Earth is spherical.
Explain how Greek astronomers calculated Earth’s size.
Describe the motion of Earth called precession.
Describe Ptolemy’s geocentric system of planetary motion.
Astronomy Around the World
Ancient Cultures and Astronomy
Babylonians, Assyrians, and Egyptians:
Determined the length of the year; Egyptians created a 365-day calendar based on the star Sirius.
Chinese Astronomers:
Recorded comets, meteors, and solar spots, and developed their calendar.
Noted on transient stars ("guest stars").
Mayan Civilization:
Created a calendar based on Venus, with sites built for astronomical observations.
Polynesian Navigators:
Used star positions for navigation over vast ocean distances.
British Stone Circles:
Ancient peoples built structures like Stonehenge to track the motions of Sun and Moon (dating as far back as 2800 BCE).
Early Greek and Roman Cosmology
Cosmology:
Derived from Greek, it refers to the study of the universe's structure and origin.
Knowledge of a Spherical Earth:
Recognized over 2000 years ago; influenced by philosophers such as Pythagoras (circa 2500 years ago) who viewed spheres as perfect forms.
Aristotle (384–322 BCE):
Explained lunar phases as resulting from illuminated portions visible from Earth.
Noted that the Moon's shadow during lunar eclipses is always round—a key argument for a spherical shape.
Observed varying night sky visibility when traveling south, indicating Earth's curvature.
Aristarchus of Samos (310–230 BCE):
Proposed a heliocentric model (Earth orbits the Sun) but was largely dismissed.
Stellar Parallax:
The Greeks could not detect this shift in star positions due to Earth's movement, leading them to favor the geocentric model.
Astronomy Basics: Evidence of Earth’s Roundness
Observations:
Ships disappearing hull-first over the horizon.
Photographs of Earth from space show it as a sphere.
Interest in regional daylight variations at the same time, affirming sphericity.
Measurement of Earth by Eratosthenes
Eratosthenes (276–194 BCE):
First to calculate Earth's circumference using geometric methods and shadows.
Observations from Syene (directly beneath the Sun) and Alexandria (shadow cast by a column).
Calculated angle of 7° corresponding to 1/50 of Earth’s circumference, inferring total circumference as 250,000 stadia.
Accuracy of estimates varied based on the length of a stadium used.
Hipparchus and Precession
Hipparchus:
Lived in Nicaea and established a star catalog with 850 entries; introduced celestial coordinates.
Discerned changes in the north celestial pole's position—related to Earth's wobble, termed precession.
Precession:
The slow change of Earth's axial orientation, moving through a circular path over 26,000 years.
Historical reference points for the North Star changing over time.
Ptolemy’s Model of the Solar System
Claudius Ptolemy (circa 140):
Author of Almagest, consolidating astronomical knowledge, particularly from Hipparchus.
Developed a geocentric model predicting planetary positions using complex epicycles and deferents to explain retrograde motion.
Model lasted over a thousand years until challenged by Copernicus.
Retrograde Motion:
Observing outer planets appearing to reverse direction; explained in Ptolemy's model as due to combined motions of Earth and planets.
Complexity of Ptolemy’s Model:
Required numerous circles (epicycles) to explain planetary motion under the assumption of a stationary Earth.
Illustrated the mathematical genius of Ptolemy, despite the model's eventual obsolescence.