The orbit of Halley s Comet



Similar documents
Introduction to the Solar System

Unit 8 Lesson 2 Gravity and the Solar System

Lecture 13. Gravity in the Solar System

Study Guide: Solar System

Solar System Fundamentals. What is a Planet? Planetary orbits Planetary temperatures Planetary Atmospheres Origin of the Solar System

The Solar System. Source

A SOLAR SYSTEM COLORING BOOK

Planets and Dwarf Planets by Shauna Hutton

Name: Earth 110 Exploration of the Solar System Assignment 1: Celestial Motions and Forces Due in class Tuesday, Jan. 20, 2015

Background Information Students will learn about the Solar System while practicing communication skills.

Chapter 25.1: Models of our Solar System

Planetary Orbit Simulator Student Guide

UC Irvine FOCUS! 5 E Lesson Plan

Related Standards and Background Information

The Solar System. Olivia Paquette

Voyage: A Journey through our Solar System. Grades 5-8. Lesson 5: Round and Round We Go Exploring Orbits in the Solar System

THE SOLAR SYSTEM - EXERCISES 1

A Solar System Coloring Book

Copyright 2006, Astronomical Society of the Pacific

Lecture 12: The Solar System Briefly

Vocabulary - Understanding Revolution in. our Solar System

USING MS EXCEL FOR DATA ANALYSIS AND SIMULATION

Astronomy 1140 Quiz 1 Review

Pocket Solar System. Make a Scale Model of the Distances in our Solar System

Pluto Data: Numbers. 14b. Pluto, Kuiper Belt & Oort Cloud. Pluto Data (Table 14-5)

The Layout of the Solar System

LER Ages. Grades. Solar System. A fun game of thinking & linking!

Our Planetary System. Earth, as viewed by the Voyager spacecraft Pearson Education, Inc.

1. Title: Relative Sizes and Distance in the Solar System: Introducing Powers of Ten

The Solar System. Unit 4 covers the following framework standards: ES 10 and PS 11. Content was adapted the following:

The Main Point. Lecture #34: Solar System Origin II. Chemical Condensation ( Lewis ) Model. How did the solar system form? Reading: Chapter 8.

Discover the planets of our solar system. In 90 minutes through the universe. On a hiking path between Ehrenfriedensdorf and Drebach

1 A Solar System Is Born

Solar System. 1. The diagram below represents a simple geocentric model. Which object is represented by the letter X?

From Aristotle to Newton

Chapter 12 Asteroids, Comets, and Dwarf Planets. Asteroid Facts. What are asteroids like? Asteroids with Moons Asteroids and Meteorites

NASA Explorer Schools Pre-Algebra Unit Lesson 2 Student Workbook. Solar System Math. Comparing Mass, Gravity, Composition, & Density

Science Standard 4 Earth in Space Grade Level Expectations

NOTES: GEORGIA HIGH SCHOOL SCIENCE TEST THE SOLAR SYSTEM

The Solar System: Cosmic encounter with Pluto

UNIT V. Earth and Space. Earth and the Solar System

HONEY, I SHRUNK THE SOLAR SYSTEM

Earth in the Solar System

Group Leader: Group Members:

A.4 The Solar System Scale Model

EDMONDS COMMUNITY COLLEGE ASTRONOMY 100 Winter Quarter 2007 Sample Test # 1

Chapter 5: Circular Motion, the Planets, and Gravity

Grade 6 Standard 3 Unit Test A Astronomy. 1. The four inner planets are rocky and small. Which description best fits the next four outer planets?

Newton s Law of Gravity

L3: The formation of the Solar System

1.1 A Modern View of the Universe" Our goals for learning: What is our place in the universe?"

Name: João Fernando Alves da Silva Class: 7-4 Number: 10

astronomy A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times.

Chapter 9 Asteroids, Comets, and Dwarf Planets. Their Nature, Orbits, and Impacts

Page. ASTRONOMICAL OBJECTS (Page 4).

Astronomy Club of Asheville October 2015 Sky Events

Summary: Four Major Features of our Solar System

Solar System Overview

Earth Is Not the Center of the Universe

Lecture 7 Formation of the Solar System. Nebular Theory. Origin of the Solar System. Origin of the Solar System. The Solar Nebula

Halliday, Resnick & Walker Chapter 13. Gravitation. Physics 1A PHYS1121 Professor Michael Burton

Name Class Period. F = G m 1 m 2 d 2. G =6.67 x Nm 2 /kg 2

Chapter 7 Our Planetary System. What does the solar system look like? Thought Question How does the Earth-Sun distance compare with the Sun s radius

Astronomy Notes for Educators

Toilet Paper Solar System

Cosmic Journey: A Solar System Adventure General Information

7. Our Solar System. Planetary Orbits to Scale. The Eight Planetary Orbits

THE SOLAR SYSTEM. Worksheets UNIT 1. Raül Martínez Verdún

2. Orbits. FER-Zagreb, Satellite communication systems 2011/12

Chapter 1: Our Place in the Universe Pearson Education Inc., publishing as Addison-Wesley

Chapter 7 Our Planetary System. Agenda. Intro Astronomy. Intro Astronomy. What does the solar system look like? A. General Basics

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: UNIVERSE AND SOLAR SYSTEM (Approximate Time 3 Weeks)

AE554 Applied Orbital Mechanics. Hafta 1 Egemen Đmre

Vagabonds of the Solar System. Chapter 17

4 HOW OUR SOLAR SYSTEM FORMED 890L

Solar System Facts & Fun

The Solar System. A Collaborative Science Activity for Key Stage 2. Teacher s Notes. Procedure

So What All Is Out There, Anyway?

Solar System Formation

Name Class Date. true

Solar System Fact Sheet

Lab 6: Kepler's Laws. Introduction. Section 1: First Law

Periods of Western Astronomy. Chapter 1. Prehistoric Astronomy. Prehistoric Astronomy. The Celestial Sphere. Stonehenge. History of Astronomy

How did the Solar System form?

Lecture 19: Planet Formation I. Clues from the Solar System

Perspective and Scale Size in Our Solar System

TO GO TO ANY OF THE PAGES LISTED BELOW, CLICK ON ITS TITLE

Douglas Adams The Hitchhikers Guide to the Galaxy

Voyage: A Journey through our Solar System. Grades 5-8. Lesson 1: Our Solar System

A Modern View of the Universe

4 HOW OUR SOLAR SYSTEM FORMED 1020L

Our Solar System Scavenger Hunt Activity

7 Scale Model of the Solar System

A = 6561 times greater. B. 81 times greater. C. equally strong. D. 1/81 as great. E. (1/81) 2 = 1/6561 as great.

The Gravitational Field

Welcome to Class 4: Our Solar System (and a bit of cosmology at the start) Remember: sit only in the first 10 rows of the room

STUDY GUIDE: Earth Sun Moon

Lecture 10 Formation of the Solar System January 6c, 2014

Out of This World Classroom Activity

Class 2 Solar System Characteristics Formation Exosolar Planets

Transcription:

The orbit of Halley s Comet Given this information Orbital period = 76 yrs Aphelion distance = 35.3 AU Observed comet in 1682 and predicted return 1758

Questions: How close does HC approach the Sun? What is the orbital eccentricity? From Kepler s 3 rd law: P 2 (yr) = a 3 (AU) So, a 3 (AU) = 76 x 76 = 5776 Hence a(au) = (5776) 1/3 = 17.94 By definition: perihelion distance + aphelion distance = 2a So, we have: Perihelion distance = 2a aphelion distance = 2x17.94 35.3 Which gives Perihelion distance = 0.58 (AU) Closer than orbit of Venus to the Sun

Definition: Eccentricity (e) e = OF / a OF Aphelion (35.3 AU) a Sun 0.58 AU Perihelion distance perihelion a = 17.94 AU By construction: a = perihelion distance + OF Hence: OF = a perihelion distance = 17.94 0.58 = 17.26 AU And, accordingly, eccentricity e = 17.26 / 17.94 = 0.96

From last class Kepler s laws of Planetary Motion 1 st law: The planets revolve around the Sun along elliptical orbits with the Sun at one focus 2 nd law: A line drawn from the planet to the Sun sweeps out equal areas in equal time 3 rd law: The square of a planets orbital period P is proportional to the cube of its orbital semimajor axis a P 2 (yr) = a 3 (AU)

Last seen in 1986 back in 2061 OF Perihelion distance Aphelion a Sun perihelion Summing up For Halley s comet Orbital period = 76 years Semi-major axis a = 17.94 AU Perihelion distance = 0.58 AU Aphelion distance = 35.3 AU Sun displacement from center OF = 17.26 AU eccentricity e = 0.96

Isaac Newton (1643-1727) Mathematician, Alchemist Biblical Scholar Physicist Master of the Mint Basically a spherically clever guy

Nature and Nature's laws lay hid in night: God said, Let Newton be! and all was light Alexander Pope F gravity G m M 2 R

Newton s genius Same physics everywhere in the lab, in the Solar System and anywhere else in the Universe in other words we can measure and understand the physics of the cosmos around us He argued: The rules describing the acceleration of objects falling on the Earth can also describe the motion of the planets Hypothesis: Newton, 1687: There is a gravitational attraction between all of the planets and the Sun

Keeping the planets in their place Newton s 1 st law of motion A body will remain at rest or in constant motion along a straight line path unless acted upon by an external force In reality, a planet is continuously accelerated towards the Sun by a gravitational force It is this continuous gravitational interaction that causes a planet to follow an elliptical orbit rather than a straight line path through space

Hammer Time When the athlete lets go of the tether, the ball flies off along a straight line path it doesn t keep going in a circle the tether is our gravitational pull analog

In each second the Moon falls 1.4 mm towards the Earth (away from straight line path) and moves 1 km around its orbit the Moon is continuously falling towards Earth, or more correctly from the straight line path it would otherwise have if there were no gravity Moon Path of Moon without gravity F g Path of Moon with gravity (orbit) Earth Not only does gravity explain planetary orbits, it also explains Kepler s 2 nd and 3 rd laws

Kepler s 3rd law. Newton style Cutting to the chase - Newton showed: P 2 /a 3 = K = 4p 2 / G(M Sun + M Planet ) In other words, Newton found that the constant K in K3 is related to the system mass Units are now kilograms, meters and seconds (the SI units of measure) G is the universal gravitational constant

The Moons of Mars: Phobos and Deimos

Phobos Period = 7.656 hours Orbital radius = 9400 km Moon diameter is about 20 km Discovered by Asaph Hall in 1877

Weighing Mars M Mars + M phobos = (4p 2 ) a 3 / G P 2 Kepler s 3 rd law with Newton s modification Can safely assume M Mars >> M Phobos so, using SI units (meters, sec., kg) M Mars = (4p 2 ) (9.4x10 6 ) 3 / G (7.656 x 3600) 2 = 6.6 x 10 23 kg = 1/10 th M Earth

Not just for planets Provided a measure of the size of the orbit (a) and the orbital period (P) can be made K3 as formulated by Newton can be used to find the masses of astronomical objects.. Later on we will weigh the stars as well as the entire Milky Way Galaxy using K3

We now have a set of tools and laws to describe: 1. Motion on the sky the celestial sphere (ecliptic) 2. The distances to the planets and the scale of the Solar System Copernicus s method for inferior planets and the Big Result formula 3. Orbital shape semi-major axis and eccentricity 4. Planetary motion Kepler s three laws 5. The mass of a planet if it has a moon Newton s refinement to K3 Our next task is to take an inventory of the Solar System what exactly is it and what kind of objects does it contain?

The contents The Solar System is a dynamic collection of many hundreds of thousands of objects: The Sun, planets, dwarf planets, moons, asteroids, comets, Kuiper-belt objects, meteoroids, dust grains. Also: magnetic fields, radiation (light), cosmic rays The planets are the largest objects (next to the Sun) in the Solar System but the definition for planetary status is not simple (or even agreed upon) Eight classical planets are recognized: Mercury Neptune and five dwarf planets: Ceres, Pluto, Eris, Makemake & Haumea

Inner solar system planets Outer solar system planets Dwarf planets

From last class Discussed Newton s result WRT Kepler s 3 rd law observations of period and orbit size enable derivation of system mass our astronomical weigh scale Discussed the scale and extent of the Solar System - Introduced the Kuiper Belt and Oort Cloud regions of the outer Solar System Kuiper belt = disc-like distribution of small ice/rock worlds beyond Pluto stretches out to ~ 20,000 AU Oort cloud = outer most boundary of the Solar System (where gravity of the Sun is less than the other stars in the rest of the galaxy) - located at ~ 100,000 AU from the Sun

200,000 AU The scale of the Solar System Oort Cloud KB Oort Cloud named after Jan Oort (1950) vast reservoir of comets surrounding Sun (spherical halo of objects) Comets can enter the inner solar system at any angle Kuiper Belt Sun Pluto 40 AU 20,000 AU Kuiper Belt named after Gerald Kuiper (1951) disk like distribution of large ice / rock objects - with Pluto being the first such object discovered (1930)

Light travel time across the Oort Cloud Kuiper belt distance velocity time OOTETK Velocity = speed of light Distance ~ 200,000 AU Meters in 1 AU Time = distance / velocity = 200,000 x 1.496 x 10 11 / 3 x 10 8 = 9.97 x 10 7 seconds = 3.16 years The solar system is BIG!!... Way big

By any other name. Conditions for planetary status: IAU (August 2006) definition: International Astronomical Union 1. Object must orbit the Sun 2. Large enough to be spherical through its own gravity (this is a size / mass constraint) 3. Must have cleared its region of the solar system of other smaller objects i.e., it is the dominant gravitational object in its region

Dwarf Planets Minor planet designation 134340 An object that satisfies conditions 1 and 2 for a planet but not condition 3 Dwarf planets presently recognized: Ceres formerly the largest asteroid» (historically a former planet) Pluto formerly a planet (discovered 1930) Eris discovered 2003 Makemake - discovered 2005 Haumea discovered 2004 Let s just have his head and be done with it

Moon Planets Haumea Dwarf planets Pluto Makemake Ceres Eris

The Solar System Ceres (dwarf planet) 134340 Pluto 136199 Eris Makemake Haumea Physical properties

The Main Components Are: Sun The nearest star to us. ~ 8% of all stars are Sun-like stars Accounts for 99.9% of the mass of the solar system Planets Terrestrial planets: Mercury Mars Small, rocky (metal core) worlds with orbits less than 2 AU from the Sun Jovian planets: Jupiter Neptune Large, mostly gas-giant planets with orbits greater than 5 AU from the Sun

Outer Solar System Inner Solar System Terrestrial planets: closely packed orbits Small, rock/iron worlds Jovian planets: widely spaced orbits Large, gas giant worlds

Dwarf Planets Ceres aside DPs have orbits beyond Neptune Pluto is essentially the first of the Dwarf Planets Have orbits beyond 35 AU Also called Made predominantly of rock and ice Plutoids Sizes smaller than Earth s Moon (< 3000 km) It is possible that large (Earth-sized) DPs exist but none have so far been detected Move in the Kuiper Belt region and can undergo collisions with KBOs producing cometary fragments Presently 5 Dwarf Planets officially recognized, dozens, even many hundreds more awaiting discovery

2390 km Greek Goddess Ruler of the underworld Hawaiian Gods of childbirth and fertility Roman Goddess