PHYS 162 Class 31 Understanding Planetary Motion Use experimental observations (made prior to telescopes) to understand motion of the planets. Period is.

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PHYS 162 Class 31 Understanding Planetary Motion Use experimental observations (made prior to telescopes) to understand motion of the planets. Period is “easy”, distances and orbit shape are “hard” Leads to Kepler’s 3 laws of planetary motion Provides experimental observations which are later explained by physics developed by Galileo, Newton and others

PHYS 162 Class 32 Models of the Solar System Ptolemaic - Geocentric Earth at center and motionless Sun and other planets orbit the Earth on circles within circles. Think Tilt-a- Whirl at Cornfest

PHYS 162 Class 33 Copernican - Heliocentric Sun at center All planets move about Sun on circles on circles Earth revolves on axis once per day Catholic Church adopts Ptolemaic as “revealed truth” in 13th Century (when first Universities in Europe began). Copernican model published in 1543 with detailed comparisons to observations (after Copernicus’ death so Church would not punish him)

PHYS 162 Class 34 Copernican vs Geocentric vs Catholic Church Bruno was burned at the stake in 1600 in Rome for stating Copernicus was correct "Innumerable suns exist; innumerable earths revolve around these suns in a manner similar to the way the seven planets revolve around our sun. Living beings inhabit these worlds." — Giordano Bruno Campo d’Fiore Rome also has farmer’s market and 4 nice inexpensive restaurants

PHYS 162 Class 35 Other Models Tycho Brahe’s - Earth at center but other planets orbit the Sun (effectively the same as Copernican) Kepler’s - Sun at center with planets orbiting the Sun in elliptical paths CORRECT Differentiate models by comparing predictions with observations SCIENTIFIC METHOD need best observations as possible

PHYS 162 Class 36 Brahe and Kepler Brahe led team which collected data on position of planets ( no telescopes) Kepler (mathematician) hired by Brahe to analyze data. Determined 3 Laws of planetary motion ( ) Input - 20 years of data on: angular position of planets approximate distances from Earth (accurate relative distances) Few “modern” tools (no calculus, no graph paper, no log tables), just Euclidan geometry

PHYS 162 Class 37 Observations of Brahe Brahe was a Danish nobleman who became famous after observing a supernova and showing it was “far away” Danish king provided funding and an island where Brahe set up an observatory – no telescopes just (essentially) sextants - that is long sticks to measure angles which could be flipped to measure both E-W and N-S angle at same time

PHYS 162 Class 38

9 Apparent Shift = Parallax Moving observer sees fixed objects shift Near objects shift more than far objects Due to change in observation point  our eyes for depth perception. angle A angle B Earth Geocentric parallax base

PHYS 162 Class 310 Sources of Parallax Heliocentric parallax: sun as base. Photos with telescope at two different seasons  use later for stars Geocentric parallax: earth as base. Measure two or more times in one night. Use for planets  Brahe’s data had distances to planets plus position in sky

PHYS 162 Class 311 Kepler’s Laws of Motion Kepler: correct orbital shape and determined some relationships between the orbits of different planets Big step: Earth’s orbit about the Sun also wasn’t a circle – mostly he used relative location of Mars after repeated orbits around the Sun (Mars is close and so most accurate measurements)

PHYS 162 Class 412 Kepler’s Laws of Planetary Motion (1630) FIRST LAW: The orbit of a planet is an ellipse with the sun at one focus. A line connecting the two foci in the ellipse always has the same length.

PHYS 162 Class 413 Kepler’s Second Law The line joining a planet and the sun sweeps equal areas in equal time. The planet moves slowly here. The planet moves quickly here.

PHYS 162 Class 414 Kepler’s Third Law The square of a planet’s period is proportional to the cube of the length of the orbit’s semimajor axis. Mathematically, T 2 /a 3 = constant.(=1 if use 1 Earth year and 1 AU as units) The constant is the same for all objects orbiting the Sun  same process determines all planets’ motions semimajor axis: a direction of orbit The time for one orbit is one period: T

PHYS 162 Class 415 Planetary Characteristics Mean Distance from Sun Sidereal Orbital Period AUPePe Mercury Venus Earth1.000 Mars Jupiter Saturn Uranus Neptune

PHYS 162 Class 416 Third Law Example Jupiter compared to Earth If we measure that it takes Jupiter 11.9 years to orbit the Sun then: distance 3 (Jupiter-Sun) = period 2 distance = period 2/3 distance = (11.9*11.9) 1/3 distance = (142) 1/3 = 5.2 AU

PHYS 162 Class 417 Kepler: determined the motion of the planets. Did not address WHY. Simply what curve best matched orbits and some arithmetical relationships WHY: determined by physicists like Galileo and Newton. Needed to develop Physics as a science: understand motion, forces, and gravity

162 Class 418 Movie – Cosmic Voyage Looks at the Universe  increasing distance scales. to billions of light years  decreasing distance scales. to subnuclear scales Looks at time evolution of Universe over billions of years  telescopes look far away are looking back in time  accelerators like Fermilab are reproducing how the Universe in the first moments after creation (Rocky Kolb from Fermilab) reminder: 2 EC points for seeing movie. Pass around signup sheet. Up to 10 points for a paper on any of the movies and can hand in two such papers (movie and/or observatory visit