NATS 101 Updates Add your name to Class ListServe! First QUIZ on today Some textbooks at Park & University Book store 1st anniversary of Katrina this week.

Slides:



Advertisements
Similar presentations
Understanding Heat Transfer, Conduction, Convection and Radiation.
Advertisements

MET 112 Global Climate Change
PHYSICS 103: Lecture 20 Blackbody Radiation Light Bulbs Agenda for Today:
Woodstoves 1 Woodstoves and lightbulbs. Woodstoves 2 Introductory Question Which is more effective at heating a room: Which is more effective at heating.
1 NATS 101 Lecture 6 Greenhouse Effect and Earth-Atmo Energy Balance.
1 NATS 101 Lecture 4 Temperature and Heat Transfer.
Chapter 22 Heat Transfer.
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.
1 NATS 101 Lecture 5 Radiation. 2 Review Items Heat Transfer Latent Heat.
1 NATS 101 Lecture 4 Temperature and Heat Transfer.
Solar Radiation Emission and Absorption
4” by 6” Cards Today’s assignment Name, SID – legible penmanship What worked What didn’t and needs clarification.
1 NATS 101 Lecture 6 Greenhouse Effect and Earth-Atmo Energy Balance.
MET 60: Chapter: 4 (W&H) and 2 (Stull) Radiative Transfer Dr. Craig Clements San José State University.
Phy100: Heat transport Three basic forms of thermal heat transport
Light Astronomy 315 Professor Lee Carkner Lecture 4.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 2 The Earth’s Energy Balance Dr. Craig Clements San José State University Outline.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 7 “Warming the Earth and Atmosphere” Dr. Eugene Cordero San Jose.
1 NATS 101 Lecture 5 Radiation. 2 Review Items Heat Transfer Latent Heat.
NATS 101 Updates Add your name to Class ListServe! First QUIZ on Thursday Review session tomorrow at ~5PM –Location TBD. Will be announced via Listserve.
Heat & Heat Transfer Heat: Heat is energy! Heat is the energy transferred (passed) from a hotter object to a cooler object. Heat Transfer: The transfer.
MECHANISMS OF HEAT TRANSFER
Thermal Energy Chapter 14. Key Ideas  What does temperature have to do with energy?  What makes things feel hot or cold?  What affects the rate that.
Radiation, Insolation, and Energy Transfer. Solar Radiation: Sun to Earth Speed of light: 300,000 km/second (186,000 miles/sec.) Distance to Earth: 150.
PHYSICS 103: Lecture 17 Agenda for Today: Temperature and Heat
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.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 2 The Earth’s Energy Balance Dr. Eugene Cordero San Jose State University Outline.
1 ATMO 336 Weather, Climate and Society Heat Transfer.
Light and Spectroscopy. Light  Charges interact via electric and magnetic forces  Light is a repetitive disturbance in these forces! Electromagnetic.
AOS February 19/21 Energy Transfer. Four mechanisms of transfer Conduction Convection Advection Radiation.
How to Make Starlight (part 1) Chapter 7. Origin of light Light (electromagnetic radiation) is just a changing electric and magnetic field. Changing electric.
Solar Energy and Energy Balance in the Atmosphere.
What is temperature? Measure of the average random kinetic energy of the molecules of a substance Physical property that determines the direction of heat.
II. Global Energy Balance. A. Electromagnetic Radiation: self-propagating electric and magnetic waves. Or …. Radiation transmitted through the vacuum.
Spectra. White Light Light from many colors mixes to form white light. Different colors have different wavelengths. Shorter wavelengths bend more through.
What is light? Light can act either like a wave or like a particle Particles of light are called photons.
Atoms & Starlight (Chapter 6).
Do Now: Based on the notes from last week, what is the difference between temperature and heat?
1 NATS 101 Lecture 4 TR Radiation Selective Absorption.
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.
NATS 101 Section 13: Lecture 5 Radiation. What causes your hand to feel warm when you place it near the pot? NOT conduction or convection. Why? Therefore,
Lecture 2: Heat and radiation in the atmosphere. TEMPERATURE… is a measure of the internal heat energy of a substance. The molecules that make up all.
Topic 5 Energy. Energy is the ability to do work or cause change Kinetic energy: energy of motion  faster objects have more kinetic energy Temperature.
Electromagnetic Radiation, Atomic Structure & Spectra.
1 NATS 101 Updates Add your name to Class ListServe! –Still missing 100 students First Quiz next Thursday Practice Quiz today.
NATS From the Cosmos to Earth Light as a Wave For a wave, its speed: s = l x f But the speed of light is a constant, c. For light: l x f = c The.
DO NOW: Heat Transfer. What type of heat transfer is shown?
On a hot sunny day, did you ever see cars, buildings, or other objects appear to shimmer or waver on the other side of a street or parking lot? What causes.
Types of HEAT Energy Transfers CONDUCTION Objects are in direct contact. Heat energy transfers when particles collide or objects in contact are TOUCHING.
Major Concepts of Physics PHY102 – Lecture #  Syracuse University Lecture #10 Do cold solids emit light? February 24 th Spring 2016 Prof. Liviu.
Heat Transfer How heat gets from one place to another.
TOPIC 5: ENERGY.
Heat & Heat Transfer Heat: Heat is energy! Heat is the energy transferred (passed) from a hotter object to a cooler object. Heat Transfer: The transfer.
Electromagnetic Radiation
NATS 101 Updates Add your name to Class ListServe!
NATS 101 Lecture 5 Radiation
NATS 101 Lecture 6 Greenhouse Effect and Earth-Atmo Energy Balance
NATS 101 Updates Add your name to Class ListServe!
Review Items Heat Transfer Latent Heat
620 cal/g 80 cal/g 540 cal/g 80 cal/g 540 cal/g 620 cal/g
Energy Transfer Through Heat
NATS 101 Updates Add your name to Class ListServe!
NATS 101 Updates Add your name to Class ListServe!
5.2 Properties of Light Our goals for learning What is light?
Temperature Is a property of an object which determines the direction of net heat flow when an object is placed in contact with some other object. Heat.
NATS 101 Updates Add your name to Class ListServe! First QUIZ on today
Chapter 2 Energy in transit
17.2 – Heating the atmosphere – Part I
Presentation transcript:

NATS 101 Updates Add your name to Class ListServe! First QUIZ on today Some textbooks at Park & University Book store 1st anniversary of Katrina this week Quick update on Ernesto & John

NATS 101 Lecture 4 Radiation

What is Temperature? Microscopic View Energy due to random jiggling of molecules Related to average molecular speed; 500 m/s (=1100 mph) at room temperature for air

Modes of Heat Transfer Williams, p. 19 Latent Heat

Take Home Concepts Heat-Energy transfer due to temperature differences Four modes of heat transfer Conduction – molecule to molecule Convection – transport of fluid Radiation – electromagnetic waves Latent Heat – energy of phase changes

Modes of Heat Transfer Energy is only converted from one form to another or transferred from one place to another. Energy is transferred from hot to cold. Conduction - Molecules colliding; most efficient at interface. Convection - Requires movement of a fluid or gas.

Radiation Any object that has a temperature greater than 0 K, emits radiation. This radiation is in the form of electromagnetic waves, produced by the acceleration of electric charges. These waves don’t need matter in order to propagate; they move at the “speed of light” (3x10 5 km/sec) in a vacuum.

Electromagnetic Waves Two important aspects of waves are: –What kind: Wavelength or distance between peaks. –How much: Amplitude or distance between peaks and valleys. Wavelength AmplitudeFrequency

Why Electromagnetic Waves? Radiation has an Electric Field Component and a Magnetic Field Component –Electric Field is Perpendicular to Magnetic Field

Photons NOT TO CONFUSE YOU, but… Can also think of radiation as individual packets of energy or PHOTONS. In simplistic terms, radiation with –shorter wavelengths corresponds to photons with more energy and –higher wave amplitude to more BB’s per second

Electromagnetic Spectrum WAVELENGTH Danielson, Fig Wavelengths of Meteorology Significance

Emitted Spectrum White Light from Flash Light PurpleGreen Red Emitted radiation has many wavelengths. Prism (Danielson, Fig. 3.14)

Emitted Spectrum Energy from Sun is spread unevenly over all wavelengths. Wavelength Energy Emitted Emission spectrum of Sun Ahrens, Fig. 2.7

Wien’s Law The hotter the object, the shorter the brightest wavelength. Danielson, Fig. 3.19

Wien’s Law Relates the wavelength of maximum emission to the temperature of mass MAX = (0.29  10 4  m K)  T -1 Warmer Objects => Shorter Wavelengths Sun-visible light MAX = (0.29  10 4  m K)  (5800 K) -1  0.5  m Earth-infrared radiation MAX = (0.29  10 4  m K)  (290 K) -1  10  m

Wien’s Law What is the radiative temperature of an incandescent bulb whose wavelength of maximum emission is near 1.0  m ? Apply Wien’s Law: MAX = (0.29  10 4  m K)  T -1 Temperature of glowing tungsten filament T= (0.29  10 4  m K)  ( MAX ) -1 T= (0.29  10 4  m K)  (1.0  m) -1  2900K

Stefan-Boltzmann’s (SB) Law The hotter the object, the more radiation emitted. When the temperature is doubled, the emitted energy increases by a factor of 16! Stefan-Boltzmann’s Law E= (5.67  Wm -2 K -4 )  T 4 E=2  2  2  2=16 4 times Sun Temp: 6000K Earth Temp: 300K Aguado, Fig. 2-7

How Much More Energy is Emitted by the Sun per m 2 Than the Earth? Apply Stefan-Boltzman Law The Sun Emits 160,000 Times More Energy per m 2 than the Earth, Plus Its Area is Mucho Bigger (by a factor of 10,000)!

Radiative Equilibrium Radiation absorbed by an object increases the energy of the object. –Increased energy causes temperature to increase (warming). Radiation emitted by an object decreases the energy of the object. –Decreased energy causes temperature to decrease (cooling).

Radiative Equilibrium (cont.) When the energy absorbed equals energy emitted, this is called Radiative Equilibrium. The corresponding temperature is the Radiative Equilibrium Temperature.

Key Points Radiation is emitted from all objects that have temperatures warmer than absolute zero (0 K). Wien’s Law: wavelength of maximum emission MAX = (0.29  10 4  m K)  T -1 Stefan-Boltzmann Law: total energy emission E= (5.67  W/m 2 )  T 4

Key Points Radiative equilibrium and temperature Energy In = Energy Out (Eq. Temp.) Three modes of heat transfer due to temperature differences. Conduction: molecule-to-molecule Convection: fluid motion Radiation: electromagnetic waves

Reading Assignment Ahrens Pages Problems 2.7, 2.9, 2.10, 2.11, 2.12