Astronomy 1010 Planetary Astronomy Fall_2015 Day-19.

Slides:



Advertisements
Similar presentations
Universe Eighth Edition Universe Roger A. Freedman William J. Kaufmann III CHAPTER 5 The Nature of Light CHAPTER 5 The Nature of Light.
Advertisements

Astronomy 201 Classical and Modern Astronomy Week 5 Slide Set 1 TAKE HOME TEST 3 HANDOUT TODAY! T3 & ADLER REPORTS DUE in 3 WKS on April 11. HW5 is due.
Introduction to Astrophysics Lecture 3: Light. Properties of light Light propagates as a wave, and corresponds to oscillations of electric and magnetic.
The Nature of Light Chapter Five.
Radiation and Spectra Chapter 5
Light and Atoms Chapter 3.
Announcements Today will be Project 1 presentation first then new material Homework Set 5: Chapter 5 # 44, 46, 47, 50, 52, 53 & 54 Exam 2 is in two weeks.
Electromagnetic Radiation Electromagnetic radiation - all E-M waves travel at c = 3 x 10 8 m/s. (Slower in water, glass, etc) Speed of light is independent.
Light Solar System Astronomy Chapter 4. Light & Matter Light tells us about matter Almost all the information we receive from space is in the form of.
Pre-Lecture Quiz: – MasteringAstronomy Ch15 pre-lecture quiz due February 17 – MasteringAstronomy Ch16 pre-lecture.
Solar Radiation Emission and Absorption
Astronomy 1 – Winter 2011 Lecture 7; January
The Nature of Light In Astronomy II. The Earth’s atmosphere absorbs most of EM spectrum, including all UV, X ray, gamma ray and most infrared. We have.
Today: Review. The idealized scientific method Based on proposing and testing hypotheses hypothesis = educated guess © 2006 Pearson Education Inc, publishing.
Astronomy 1010 Planetary Astronomy Fall_2014 Day-17.
Black Body Radiation Physics 113 Goderya Chapter(s): 7 Learning Outcomes:
Quiz 1 Each quiz sheet has a different 5-digit symmetric number which must be filled in (as shown on the transparency, but NOT the same one!!!!!) Please.
© 2004 Pearson Education Inc., publishing as Addison-Wesley Orbital Energy and Escape Velocity orbital energy = kinetic energy + gravitational potential.
Solar Spectrum. Bit of Administration …. c = 3 x 10 8 m/sec = 3 x 10 5 km/secc = 3 x 10 8 m/sec = 3 x 10 5 km/sec Reading Reading –BSNV pp
Physics 55 Monday, October 17, What light can tell us, continued 2.Application of thermal emission to greenhouse warming. 3.Doppler shift with application.
What is a Star? Wednesday, October 8 Next Planetarium Shows: Tonight 7 pm, Thurs 7 pm.
Chapter 3 Light and Matter
Blackbody Radiation & Atomic Spectra. “Light” – From gamma-rays to radio waves The vast majority of information we have about astronomical objects comes.
Chapter 3 Radiation. Units of Chapter Information from the Skies 3.2 Waves in What? The Wave Nature of Radiation 3.3 The Electromagnetic Spectrum.
Goals for Today 1.COMPARE infrared, ultraviolet, and visible electromagnetic radiation in terms of energy per photon, frequency, and wavelength 2.COMPARE.
1 Stellar Astronomy Spring_2015 Day-25.
The Big Bang Thursday, January 17.
What Can Spectroscopy Tell Us?. Atom or Molecular Fingerprints Every atom or molecule exists in its own unique energy state. This energy state is dependent.
Lecture 12 ASTR 111 – Section 002.
Chapter 5 Light: The Cosmic Messenger. 5.2 Learning from Light Our goals for learning What types of light spectra can we observe? How does light tell.
Chapter 5: Light.
Astronomy 1010-H Planetary Astronomy Fall_2015 Day-19.
Astronomy 1020 Stellar Astronomy Spring_2015 Day-17.
© 2004 Pearson Education Inc., publishing as Addison-Wesley 6. Light: The Cosmic Messenger.
1 Nature of Light Wave Properties Light is a self- propagating electro- magnetic wave –A time-varying electric field makes a magnetic field –A time-varying.
READING Unit 22, Unit 23, Unit 24, Unit 25. Homework 4 Unit 19, problem 5, problem 7 Unit 20, problem 6, problem 9 Unit 21, problem 9 Unit 22, problem.
Astronomy 101 The Solar System Tuesday, Thursday 2:30-3:45 pm Hasbrouck 20 Tom Burbine
Light 1)Exam Review 2)Introduction 3)Light Waves 4)Atoms 5)Light Sources October 14, 2002.
EOSC Radiation Balance I Goals for Today
1 Stellar Astronomy Spring_2015 Day-18.
Homework 4 Unit 21 Problem 17, 18, 19 Unit 23 Problem 9, 10, 13, 15, 17, 18, 19, 20.
Atom and Light ASTR 14: Exploring the Universe. 2 Outline Nature of Light Basic Properties of Light Atomic Structure Periodic Table of the Elements Three.
What is light? Light can act either like a wave or like a particle Particles of light are called photons.
Copyright © 2010 Pearson Education, Inc. Lecture Outline Chapter 2 Light and Matter.
Lecture 10: Light & Distance & Matter Astronomy 1143 – Spring 2014.
Atom and Light Lancelot L. Kao Updated: Jan 24, 2010.
Energy Balance. HEAT TRANSFER PROCESSES Conductive heat transfer Convective heat transfer Radiation heat transfer.
This Week (3) Concepts: Light and Earth’s Energy Balance Electromagnetic Radiation Blackbody Radiation and Temperature Earth’s Energy Balance w/out atmosphere.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 3 The Earth’s Energy Balance Dr. Eugene Cordero San Jose State University Outline.
Universe Tenth Edition Chapter 5 The Nature of Light Roger Freedman Robert Geller William Kaufmann III.
Astronomy 1010 Planetary Astronomy Fall_2015 Day-18.
Electromagnetic Radiation, Atomic Structure & Spectra.
Astronomy 1010-H Planetary Astronomy Fall_2015 Day-18.
Blackbody Radiation A blackbody is something that absorbs all radiation that shines on it Are all blackbodies black? - no!! - imagine a box full of lava.
Astronomy 1020-H Stellar Astronomy Spring_2016 Day-15.
Lecture Outlines Astronomy Today 8th Edition Chaisson/McMillan © 2014 Pearson Education, Inc. Chapter 3.
Light and The Electromagnetic Spectrum Why do we have to study “light”?... Because almost everything in astronomy is known because of light (or some.
Radiation in Astronomy Electromagnetic Radiation I. Electromagnetic Radiation (EM) (EM) Energy travels through space as EM. $ Electromagnetic electric.
The Solar System Lesson2 Q & A
Blackbody Radiation/ Planetary Energy Balance
Radiation in Astronomy
Blackbody Radiation/ Planetary Energy Balance
Homework #3 will be posted on Wednesday
Electromagnetic Radiation
Chapter 15 Surveying the Stars
Light: The Cosmic Messenger
Stars and Galaxies Lesson2 Q & A
Doppler Effect The Doppler Effect is the motion induced change in the observed frequency of a wave. The effect can only be observed/seen due to the relative.
5.4 Thermal Radiation 5.5 The Doppler Effect
Thermal Radiation and The Doppler Effect (5.4 & 5.5)
Presentation transcript:

Astronomy 1010 Planetary Astronomy Fall_2015 Day-19

Course Announcements Dark Sky nights – Wed. 10/7 starting at 7:30pm – at the Observatory. Exam-2 will be Friday, Oct. 9; Ch. 3, 4, & 5 SW-chapter 5 posted: due Fri. Oct. 9 No lab next week – Fall Break CHECK YOUR LAB GRADES IN D2L. If you are missing grades, and have gotten the lab back, return it so we can enter the grade. (mostly Scientific Methods, but might be others as well.)

Doppler Shifts Redshift (to longer wavelengths): The source is moving away from the observer Blueshift (to shorter wavelengths): The source is moving towards the observer  = wavelength shift o = wavelength if source is not moving v = velocity of source c = speed of light

 If you know the wavelength of light you are observing as well as the wavelength of light the object would be emitting if it were at rest, you can find the speed of the object using the Doppler effect. MATH TOOLS 5.2

i_Clicker Question Light & Spectra: Hydrogen Doppler Shift Light & Spectra: Racetrack Radar

 Temperature is a measure of the average speed of the motions of atoms.  Kelvin scale: Water freezes/boils at 273 K / 373 K.  Absolute zero is when thermal motion stops.

Emitted Light  Luminosity: amount of light leaving a source.  The amount and type of light leaving a source changes as an object heats up or cools down.  The hotter an object is, the more luminous it is.  The hotter an object is, the bluer it is.

 Dense objects emit a blackbody (or Planck) spectrum.  Continuous.  Gives light at all wavelengths.  Example: incandescent light bulb.

 For two objects of the same size, the hotter one will: Emit more total light at all wavelengths. Emit more total energy every second. Emit light at shorter wavelengths, on average.

Stefan’s Law  Flux is the total amount of energy emitted per square meter every second (the luminosity per area).  Then: where T is the temperature, F is the flux, and  (sigma) is called the Stefan- Boltzmann constant.  Hotter objects emit much more energy (per square meter per second) than cool objects.

Wien’s Law  The peak wavelength of a blackbody is inversely proportional to its temperature.  Peak wavelength peak : the wavelength of light of a blackbody that is emitted the most.  Here the wavelength is in nanometers and the temperature is in kelvin.  “Hotter means bluer.”

i_Clicker Question Light & Spectra: Blackbody Curve Laws Light & Spectra: Blackbody Curve Temperatures

 Brightness is the amount of light arriving at a particular place.  Decreases as the distance from a light source increases, obeying an inverse square law.  The light spreads out over a greater area.

i_Clicker Question Light & Spectra: Inverse Square Flux

Equilibrium Temperature Balance between absorbed and radiated energy. Albedo (reflectance) of a planet. a = 1: 100% reflection a = 0 : 100% absorption Energy absorbed =  R 2 * L/4  d 2 * (1 – a) Energy Radiated = 4  R 2 *  T 4

 Radiation laws help figure out the equilibrium temperatures of the planets.  Distant planets are cold mainly because of the inverse square law of light.  Balance of heating and cooling.

 A stable equilibrium is a balance that is unlikely to change, while an unstable equilibrium can easily be nudged away from its balance point.  Static equilibrium involves a situation where forces are balanced and opposing each other, so nothing changes.  Dynamic equilibrium involves a situation that is always changing, but remains in balance. CONNECTIONS 5.1

 With the Stefan-Boltzmann law, you can find Earth’s flux using its average temperature of 288 K.  Using Wien’s law, you can find the Sun’s surface temperature using the fact that its peak wavelength is around 500 nm. MATH TOOLS 5.3

 The equilibrium temperature of a planet depends on the energy it receives and its albedo (a), its reflectivity. MATH TOOLS 5.4

 The equilibrium temperature of a planet depends on the energy it receives and its albedo (a), its reflectivity.  Simplifying: MATH TOOLS 5.4

PROCESS OF SCIENCE  Confirmation of an idea from different fields of science can be a strong indication of the truth of that idea.

Exam-2 To Here!