Absorptivity, Reflectivity, and Transmissivity

Save this PDF as:

Size: px
Start display at page:

Transcription

1 cen54261_ch21.qxd 1/25/4 11:32 AM Page where f l1 and f l2 are blackbody functions corresponding to l 1 T and l 2 T. These functions are determined from Table 21 2 to be l 1 T (3 mm)(8 K) 24 mm K f l l 2 T (7 mm)(8 K) 56 mm K f l Note that f l1 f l1 f f l1, since f, and f l2 f f l2 1 f l2, since f 1. Substituting, e ( ).1(1.7146).521 That is, the surface will emit as much energy at 8 K as a g surface having a constant emissivity of e.521. The emissive power of the surface is E est 4.521( W/m 2 K 4 )(8 K) 4 12,1 W/m 2 Discussion Note that the surface emits 12.1 kj of energy per second per m 2 area of the surface., W/m 2 Reflected ρ Semitransparent material Absorbed α Absorptivity, Reflectivity, and Transmissivity Everything around us constantly emits, and the emissivity represents the emission characteristics of those bodies. This means that every body, including our own, is constantly bombarded by coming from all directions over a range of wavelengths. Recall that flux incident on a surface is called ir and is denoted by. When strikes a surface, part of it is absorbed, part of it is reflected, and the remaining part, if any, is transmitted, as illustrated in Fig The fraction of ir absorbed by the surface is called the absorptivity a, the fraction reflected by the surface is called the reflectivity r, and the fraction transmitted is called the transmissivity t. That is, Absorptivity: Absorbed a, abs a 1 (21 37) Reflectivity: Reflected r, ref r 1 (21 38) Transmissivity: Transmitted t tr, t 1 (21 39) Transmitted τ FIURE The absorption, reflection, and transmission of incident by a semitransparent material. where is the energy incident on the surface, and abs, ref, and tr are the absorbed, reflected, and transmitted portions of it, respectively. The first law of thermodynamics requires that the sum of the absorbed, reflected, and transmitted energy be equal to the incident. That is, Dividing each term of this relation by yields abs ref tr (21 4) For opaque surfaces, t, and thus a r t 1 (21 41)

2 cen54261_ch21.qxd 1/25/4 11:32 AM Page CHAPTER 21 a r 1 (21 42) This is an important property relation since it enables us to determine both the absorptivity and reflectivity of an opaque surface by measuring either of these properties. These definitions are for total hemispherical properties, since represents the flux incident on the surface from all directions over the hemispherical space and over all wavelengths. Thus, a, r, and t are the average properties of a medium for all directions and all wavelengths. However, like emissivity, these properties can also be defined for a specific wavelength and/or direction. For example, the spectral directional absorptivity and spectral directional reflectivity of a surface are defined, respectively, as the absorbed and reflected fractions of the intensity of incident at a specified wavelength in a specified direction as a l, u (l, u, f) I l, abs(l, u, f) I l, i (l, u, f) and r l, u (l, u, f) I l, ref(l, u, f) I l, i (l, u, f) (21 43) Likewise, the spectral hemispherical absorptivity and spectral hemispherical reflectivity of a surface are defined as l, abs (l) l, ref (l) a l (l) and r l (l) (21 44) where l is the spectral ir (in W/m 2 mm) incident on the surface, and l, abs and l, ref are the reflected and absorbed portions of it, respectively. Similar quantities can be defined for the transmissivity of semitransparent materials. For example, the spectral hemispherical transmissivity of a medium can be expressed as l, tr (l) t l (l) (21 45) The average absorptivity, reflectivity, and transmissivity of a surface can also be defined in terms of their spectral counterparts as a l l dl r l l dl t l l dl a, r, t (21 46) l dl l dl l dl The reflectivity differs somewhat from the other properties in that it is bidirectional in nature. That is, the value of the reflectivity of a surface depends not only on the direction of the incident but also the direction of reflection. Therefore, the reflected s of a beam incident on a real surface in a specified direction will form an irregular shape, as shown in Fig Such detailed reflectivity data do not exist for most surfaces, and even if they did, they would be of little value in calculations since this would usually add more complication to the analysis than it is worth. In practice, for simplicity, surfaces are assumed to reflect in a perfectly specular or diffuse manner. In specular (or mirrorlike) reflection, the angle of reflection equals the angle of incidence of the beam. In diffuse reflection, is reflected equally in all directions, as shown in Fig. (a) (b) (c) Reflected s Reflected s Reflected FIURE Different types of reflection from a surface: (a) actual or irregular, (b) diffuse, and (c) specular or mirrorlike.

3 cen54261_ch21.qxd 1/25/4 11:32 AM Page Absorptivity, α White fireclay 2. Asbestos 3. Cork 4. Wood 5. Porcelain 6. Concrete 7. Roof shingles 8. Aluminum 9. raphite Source temperature, K FIURE Variation of absorptivity with the temperature of the source of ir for various common materials at room temperature Reflection from smooth and polished surfaces approximates specular reflection, whereas reflection from rough surfaces approximates diffuse reflection. In analysis, smoothness is defined relative to wavelength. A surface is said to be smooth if the height of the surface roughness is much smaller than the wavelength of the incident. Unlike emissivity, the absorptivity of a material is practically independent of surface temperature. However, the absorptivity depends strongly on the temperature of the source at which the incident is originating. This is also evident from Fig , which shows the absorptivities of various materials at room temperature as functions of the temperature of the source. For example, the absorptivity of the concrete roof of a house is about.6 for solar (source temperature: 578 K) and.9 for originating from the surrounding trees and buildings (source temperature: 3 K), as illustrated in Fig Notice that the absorptivity of aluminum increases with the source temperature, a characteristic for metals, and the absorptivity of electric nonconductors, in general, decreases with temperature. This decrease is most pronounced for surfaces that appear white to the eye. For example, the absorptivity of a white painted surface is low for solar, but it is rather high for infrared. α =.9 Sun α =.6 Kirchhoff s Law Consider a small body of surface area A s, emissivity e, and absorptivity a at temperature T contained in a large isothermal enclosure at the same temperature, as shown in Fig Recall that a large isothermal enclosure forms a blackbody cavity regardless of the radiative properties of the enclosure surface, and the body in the enclosure is too small to interfere with the blackbody nature of the cavity. Therefore, the incident on any part of the surface of the small body is equal to the emitted by a blackbody at temperature T. That is, E b (T ) st 4, and the absorbed by the small body per unit of its surface area is abs a ast 4 The emitted by the small body is FIURE The absorptivity of a material may be quite different for originating from sources at different temperatures. E emit est 4 Considering that the small body is in thermal equilibrium with the enclosure, the net rate of heat transfer to the body must be zero. Therefore, the emitted by the body must be equal to the absorbed by it: A s est 4 A s ast 4 Thus, we conclude that e(t ) a(t ) (21 47) That is, the total hemispherical emissivity of a surface at temperature T is equal to its total hemispherical absorptivity for coming from a blackbody at the same temperature. This relation, which greatly simplifies the analysis, was first developed by ustav Kirchhoff in 186 and is now called Kirchhoff s law. Note that this relation is derived under the condition

4 cen54261_ch21.qxd 1/25/4 11:32 AM Page 973 that the surface temperature is equal to the temperature of the source of ir, and the reader is cautioned against using it when considerable difference (more than a few hundred degrees) exists between the surface temperature and the temperature of the source of ir. The derivation above can also be repeated for at a specified wavelength to obtain the spectral form of Kirchhoff s law: e l (T ) a l (T ) (21 48) This relation is valid when the ir or the emitted is independent of direction. The form of Kirchhoff s law that involves no restrictions is the spectral directional form expressed as e l, u (T ) a l, u (T ). That is, the emissivity of a surface at a specified wavelength, direction, and temperature is always equal to its absorptivity at the same wavelength, direction, and temperature. It is very tempting to use Kirchhoff s law in analysis since the relation e a together with r 1 a enables us to determine all three properties of an opaque surface from a knowledge of only one property. Although Eq gives acceptable results in most cases, in practice, care should be exercised when there is considerable difference between the surface temperature and the temperature of the source of incident. The reenhouse Effect You have probably noticed that when you leave your car under direct sunlight on a sunny day, the interior of the car gets much warmer than the air outside, and you may have wondered why the car acts like a heat trap. The answer lies in the spectral transmissivity curve of the glass, which resembles an inverted U, as shown in Fig We observe from this figure that glass at thicknesses encountered in practice transmits over 9 percent of in the visible range and is practically opaque (nontransparent) to in the longer-wavelength infrared regions of the electromagnetic spectrum (roughly l 3 mm). Therefore, glass has a transparent window in the wavelength range.3 mm l 3 mm in which over 9 percent of solar is emitted. On the other hand, the entire emitted by surfaces at room temperature falls in the infrared region. Consequently, glass allows the solar to enter but does not allow the infrared from the interior surfaces to escape. This causes a rise in the interior temperature as a result of the energy buildup in the car. This heating effect, which is due to the nong characteristic of glass (or clear plastics), is known as the greenhouse effect, since it is utilized primarily in greenhouses (Fig ). The greenhouse effect is also experienced on a larger scale on earth. The surface of the earth, which warms up during the day as a result of the absorption of solar energy, cools down at night by radiating its energy into deep space as infrared. The combustion gases such as CO 2 and water vapor in the atmosphere transmit the bulk of the solar but absorb the infrared emitted by the surface of the earth. Thus, there is concern that the energy trapped on earth will eventually cause global warming and thus drastic changes in weather patterns. In humid places such as coastal areas, there is not a large change between the daytime and nighttime temperatures, because the humidity acts as a barrier 973 CHAPTER 21 T A s, εα, FIURE The small body contained in a large isothermal enclosure used in the development of Kirchhoff s law τ λ.4.2 Visible T E emit Thickness.38 cm.318 cm.635 cm Wavelength λ, µ m FIURE The spectral transmissivity of low-iron glass at room temperature for different thicknesses. Solar reenhouse Infrared FIURE A greenhouse traps energy by allowing the solar to come in but not allowing the infrared to go out.

5 cen54261_ch21.qxd 1/25/4 11:32 AM Page Earth s surface = s cos Earth s atmosphere n^ Sun s s s, W/m 2 FIURE Solar reaching the earth s atmosphere and the total solar irradiance. on the path of the infrared coming from the earth, and thus slows down the cooling process at night. In areas with clear skies such as deserts, there is a large swing between the daytime and nighttime temperatures because of the absence of such barriers for infrared ATMOSPHERIC AND SOLAR RADIATION The sun is our primary source of energy. The energy coming off the sun, called solar energy, reaches us in the form of electromagnetic waves after experiencing considerable interactions with the atmosphere. The energy emitted or reflected by the constituents of the atmosphere form the atmospheric. Here we give an overview of the solar and atmospheric because of their importance and relevance to daily life. Also, our familiarity with solar energy makes it an effective tool in developing a better understanding for some of the new concepts introduced earlier. Detailed treatment of this exciting subject can be found in numerous books devoted to this topic. The sun is a nearly spherical body that has a diameter of D m and a mass of m kg and is located at a mean distance of L m from the earth. It emits energy continuously at a rate of E sun W. Less than a billionth of this energy (about W) strikes the earth, which is sufficient to keep the earth warm and to maintain life through the photosynthesis process. The energy of the sun is due to the continuous fusion reaction during which two hydrogen atoms fuse to form one atom of helium. Therefore, the sun is essentially a nuclear reactor, with temperatures as high as 4,, K in its core region. The temperature drops to about 58 K in the outer region of the sun, called the convective zone, as a result of the dissipation of this energy by. The solar energy reaching the earth s atmosphere is called the total solar irradiance s, whose value is s 1373 W/m 2 (21 49) Sun 1m 2 r E b = σt 4 sun s 1m 2 (4 πr 2 )E b Earth FIURE The total solar energy passing through concentric spheres remains constant, but the energy falling per unit area decreases with increasing radius. L (4 πl 2 ) s The total solar irradiance (also called the solar constant) represents the rate at which solar energy is incident on a surface normal to the sun s s at the outer edge of the atmosphere when the earth is at its mean distance from the sun (Fig ). The value of the total solar irradiance can be used to estimate the effective surface temperature of the sun from the requirement that (4pL 2 ) s (4pr 2 ) st 4 sun (21 5) where L is the mean distance between the sun s center and the earth and r is the radius of the sun. The left-hand side of this equation represents the total solar energy passing through a spherical surface whose radius is the mean earth sun distance, and the right-hand side represents the total energy that leaves the sun s outer surface. The conservation of energy principle requires that these two quantities be equal to each other, since the solar energy experiences no attenuation (or enhancement) on its way through the vacuum (Fig ). The effective surface temperature of the sun is determined from Eq to be T sun 578 K. That is, the sun can be treated as a

Lecture 3: Global Energy Cycle

Lecture 3: Global Energy Cycle Planetary energy balance Greenhouse Effect Vertical energy balance Latitudinal energy balance Seasonal and diurnal cycles Solar Flux and Flux Density Solar Luminosity (L)

Lecture 2: Global Energy Cycle

Lecture 2: Global Energy Cycle Planetary energy balance Greenhouse Effect Vertical energy balance Solar Flux and Flux Density Solar Luminosity (L) the constant flux of energy put out by the sun L = 3.9

Teaching Energy Balance using Round Numbers: A Quantitative Approach to the Greenhouse Effect and Global Warming

Teaching Energy Balance using Round Numbers: A Quantitative Approach to the Greenhouse Effect and Global Warming Brian Blais Science and Technology Department Bryant College bblais@bryant.edu August 29,

Exercises Conduction (pages ) 1. Define conduction. 2. What is a conductor?

Exercises 22.1 Conduction (pages 431 432) 1. Define conduction. 2. What is a conductor? 3. are the best conductors. 4. In conduction, between particles transfer thermal energy. 5. Is the following sentence

Energy Balance and Temperature. Ch. 3: Energy Balance. Ch. 3: Temperature. Controls of Temperature

Energy Balance and Temperature 1 Ch. 3: Energy Balance Propagation of Radiation Transmission, Absorption, Reflection, Scattering Incoming Sunlight Outgoing Terrestrial Radiation and Energy Balance Net

Lecture 2: Global Energy Cycle

Lecture 2: Global Energy Cycle Planetary energy balance Greenhouse Effect Selective absorption Vertical energy balance Solar Flux and Flux Density Solar Luminosity (L) the constant flux of energy put out

8.5 GREENHOUSE EFFECT 8.6 GLOBAL WARMING HW/Study Packet

8.5 GREENHOUSE EFFECT 8.6 GLOBAL WARMING HW/Study Packet Required: READ Tsokos, pp 434-450 Hamper pp 294-307 SL/HL Supplemental: none REMEMBER TO. Work through all of the example problems in the texts

Emissivity: Understanding the difference between apparent and actual infrared temperatures

Emissivity: Understanding the difference between apparent and actual infrared temperatures By L. Terry Clausing, P.E. ASNT Certified NDT Level III T/IR, for Fluke Corporation Application Note Taking infrared

Solar radiation / radiative transfer The sun as a source of energy The sun is the main source of energy for the climate system, exceeding the next importat source (geothermal energy) by 4 orders of magnitude!

Equation for Global Warming

Equation for Global Warming Derivation and Application Contents 1. Amazing carbon dioxide How can a small change in carbon dioxide (CO 2 ) content make a critical difference to the actual global surface

Energy: Warming the earth and Atmosphere. air temperature. Overview of the Earth s Atmosphere 9/10/2012. Composition. Chapter 3.

Overview of the Earth s Atmosphere Composition 99% of the atmosphere is within 30km of the Earth s surface. N 2 78% and O 2 21% The percentages represent a constant amount of gas but cycles of destruction

PHYSICS 289 Experiment 3 Fall Heat transfer and the Greenhouse Effect

PHYSICS 289 Experiment 3 Fall 2006 Heat transfer and the Greenhouse Effect Only a short report is required: worksheets, graphs and answers to the questions. Introduction In this experiment we study the

The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy

Energy Balance The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy Balance Electromagnetic Radiation Electromagnetic

Warming Earth and its Atmosphere The Diurnal and Seasonal Cycles

Warming Earth and its Atmosphere The Diurnal and Seasonal Cycles Or, what happens to the energy received from the sun? First We Need to Understand The Ways in Which Heat Can be Transferred in the Atmosphere

General Physics (PHY 2130)

General Physics (PHY 2130) Lecture 34 Heat Heat transfer Conduction Convection Radiation http://www.physics.wayne.edu/~apetrov/phy2130/ Lightning Review Last lecture: 1. Thermal physics Heat. Specific

Learning goals. Good absorbers are good emitters Albedo, and energy absorbed, changes equilibrium temperature

Greenhouse effect Learning goals Good absorbers are good emitters Albedo, and energy absorbed, changes equilibrium temperature Wavelength (color) and temperature related: Wein s displacement law Sun/Hot:

Bernoulli s Principle. Application: Lift. Bernoulli s Principle. Main Points 3/13/15. Demo: Blowing on a sheet of paper

Bernoulli s Principle Demo: Blowing on a sheet of paper Where the speed of a fluid increases, internal pressure in the fluid decreases. Due to continuous flow of a fluid: what goes in must come out! Fluid

1. The most important aspects of the quantum theory.

Lecture 5. Radiation and energy. Objectives: 1. The most important aspects of the quantum theory: atom, subatomic particles, atomic number, mass number, atomic mass, isotopes, simplified atomic diagrams,

Chapter 4 Radiation from planets We consider first basic, mostly photometric radiation parameters for solar system planets which can be easily compared with existing or future observations of extra-solar

Temperature Measurement

Temperature Measurement Dr. Clemens Suter, Prof. Sophia Haussener Laboratory of Renewable Energy Sciences and Engineering Suter Temperature Measurement Mar, 2017 1/58 Motivation Suter Temperature Measurement

The Atmosphere: Structure and Temperature

Chapter The Atmosphere: Structure and Temperature Geologists have uncovered evidence of when Earth was first able to support oxygenrich atmosphere similar to what we experience today and more so, take

April 14, ESCI-61 Introduction to Photovoltaic Technology. Lecture #2. Solar Radiation. Ridha Hamidi, Ph.D.

April 14, 2010 1 ESCI-61 Introduction to Photovoltaic Technology Lecture #2 Solar Radiation Ridha Hamidi, Ph.D. April 14, 2010 2 The Sun The Sun is a perpetual source of energy It has produced energy for

Greenhouse Effect. Julia Porter, Celia Hallan, Andrew Vrabel Miles, Gary DeFrance, and Amber Rose

Greenhouse Effect Julia Porter, Celia Hallan, Andrew Vrabel Miles, Gary DeFrance, and Amber Rose What is the Greenhouse Effect? The greenhouse effect is a natural occurrence caused by Earth's atmosphere

Answers to test yourself questions Topic 8 8. Energy sources a pecific energy is the energy that can be extracted from a unit mass of a fuel while energy density is the energy that can be extracted from

Stellar Structure. Observationally, we can determine: Can we explain all these observations?

Stellar Structure Observationally, we can determine: Flux Mass Distance Luminosity Temperature Radius Spectral Type Composition Can we explain all these observations? Stellar Structure Plan: Use our general

. Advanced adiation. Gray Surfaces The gray surface is a medium whose monochromatic emissivity ( λ does not vary with wavelength. The monochromatic emissivity is defined as the ratio of the monochromatic

Composition, Structure and Energy. ATS 351 Lecture 2 September 14, 2009

Composition, Structure and Energy ATS 351 Lecture 2 September 14, 2009 Composition of the Atmosphere Atmospheric Properties Temperature Pressure Wind Moisture (i.e. water vapor) Density Temperature A measure

Thermal Systems Design MARYLAND. Fundamentals of heat transfer Radiative equilibrium Surface properties Non-ideal effects

Fundamentals of heat transfer Radiative equilibrium Surface properties Non-ideal effects Internal power generation Environmental temperatures Conduction Thermal system components 2002 David L. Akin - All

Today. Spectra. Thermal Radiation. Wien s Law. Stefan-Boltzmann Law. Kirchoff s Laws. Emission and Absorption. Spectra & Composition

Today Spectra Thermal Radiation Wien s Law Stefan-Boltzmann Law Kirchoff s Laws Emission and Absorption Spectra & Composition Spectrum Originally, the range of colors obtained by passing sunlight through

IB Physics Lesson Year Two: Standards from IB Subject Guide beginning 2016

IB Physics Lesson Year Two: Standards from IB Subject Guide beginning 2016 Planet Designer: Kelvin Climber IB Physics Standards taken from Topic 8: Energy Production 8.2 Thermal energy transfer Nature

1 A 3 C 2 B 4 D. 5. During which month does the minimum duration of insolation occur in New York State? 1 February 3 September 2 July 4 December

INSOLATION REVIEW 1. The map below shows isolines of average daily insolation received in calories per square centimeter per minute at the Earth s surface. If identical solar collectors are placed at the

UNIT FOUR SOLAR COLLECTORS

ME 476 Solar Energy UNIT FOUR SOLAR COLLECTORS Flat Plate Collectors Outline 2 What are flat plate collectors? Types of flat plate collectors Applications of flat plate collectors Materials of construction

ElectroMagnetic Radiation (EMR) Lecture 2-3 August 29 and 31, 2005

ElectroMagnetic Radiation (EMR) Lecture 2-3 August 29 and 31, 2005 Jensen, Jensen, Ways of of Energy Transfer Energy is is the the ability to to do do work. In In the the process of of doing work, energy

Physical and mathematical models of the greenhouse effect

Physical and mathematical models of the greenhouse effect My Research Questions If the Earth had no atmosphere, its average surface temperature would be about 18 C. However, the heat trapping effect of

GARP 0102 Earth Radiation Balance (Part 1)

Class 8: Earth s Radiation Balance I (Chapter 4) 1. Earth s Radiation Balance: Sun, Atmosphere, and Earth s Surface as a System 2. Electromagnetic Radiation: Shortwave vs. longwave radiation (Page 69-71)

Beer-Lambert (cont.)

The Beer-Lambert Law: Optical Depth Consider the following process: F(x) Absorbed flux df abs F(x + dx) Scattered flux df scat x x + dx The absorption or scattering of radiation by an optically active

Stefan-Boltzmann law for the Earth as a black body (or perfect radiator) gives:

2. Derivation of IPCC expression ΔF = 5.35 ln (C/C 0 ) 2.1 Derivation One The assumptions we will make allow us to represent the real atmosphere. This remarkably reasonable representation of the real atmosphere

Most of the energy from the light sources was transferred to the sand by the process of A) conduction B) convection C) radiation D) transpiration

1. Light and other forms of electromagnetic radiation are given off by stars using energy released during A) nuclear fusion B) conduction C) convection D) radioactive decay 2. At which temperature would

Law of Heat Transfer

Law of Heat Transfer The Fundamental Laws which are used in broad area of applications are: 1. The law of conversion of mass 2. Newton s second law of motion 3. First and second laws of thermodynamics

PHYSICS OF FOIL. HEAT GAIN/LOSS IN BUILDINGS. Up Heat Flow. Down Heat Flow. Side Heat Flow

HEAT GAIN/LOSS IN BUILDINGS There are three modes of heat transfer: CONDUCTION, CONVECTION, and RADIATION (INFRA-RED). Of the three, radiation is the primary mode; conduction and convection are secondary

HEAT BUDGET AND RADIATION A Heat Budget 1 Black body radiation Definition. A perfect black body is defined as a body that absorbs all radiation that falls on it. The intensity of radiation emitted by a

Chapter 22: Uses of Solar Energy

Chapter 22: Uses of Solar Energy Goals of Period 22 Section 22.1: To describe three forms of energy derived from solar energy water power, wind power, and biomass Section 22.2: To illustrate some uses

Chapter 7. Solar Cell

Chapter 7 Solar Cell 7.0 Introduction Solar cells are useful for both space and terrestrial application. Solar cells furnish the long duration power supply for satellites. It converts sunlight directly

Electromagnetic Radiation. Physical Principles of Remote Sensing

Electromagnetic Radiation Physical Principles of Remote Sensing Outline for 4/3/2003 Properties of electromagnetic radiation The electromagnetic spectrum Spectral emissivity Radiant temperature vs. kinematic

Electromagnetic spectra

Properties of Light Waves, particles and EM spectrum Interaction with matter Absorption Reflection, refraction and scattering Polarization and diffraction Reading foci: pp 175-185, 191-199 not responsible

What Is Air Temperature?

2.2 Read What Is Air Temperature? In Learning Set 1, you used a thermometer to measure air temperature. But what exactly was the thermometer measuring? What is different about cold air and warm air that

Opacity and Optical Depth

Opacity and Optical Depth Absorption dominated intensity change can be written as di λ = κ λ ρ I λ ds with κ λ the absorption coefficient, or opacity The initial intensity I λ 0 of a light beam will be

Section 2: The Atmosphere

Section 2: The Atmosphere Preview Classroom Catalyst Objectives The Atmosphere Composition of the Atmosphere Air Pressure Layers of the Atmosphere The Troposphere Section 2: The Atmosphere Preview, continued

Spectral reflectance: When the solar radiation is incident upon the earth s surface, it is either

Spectral reflectance: When the solar radiation is incident upon the earth s surface, it is either reflected by the surface, transmitted into the surface or absorbed and emitted by the surface. Remote sensing

ME 476 Solar Energy UNIT THREE SOLAR RADIATION

ME 476 Solar Energy UNIT THREE SOLAR RADIATION Unit Outline 2 What is the sun? Radiation from the sun Factors affecting solar radiation Atmospheric effects Solar radiation intensity Air mass Seasonal variations

Simultaneous Conduction and Radiation Energy Transfer

Simultaneous Conduction and Radiation Energy Transfer Radiant energy can transfer from a colder to a warmer radiator. ###########, PhD Chemical Process Control Systems Engineer, PE TX & CA Abstract The

K20: Temperature, Heat, and How Heat Moves

K20: Temperature, Heat, and How Heat Moves Definition of Temperature Definition of Heat How heat flows (Note: For all discussions here, particle means a particle of mass which moves as a unit. It could

Thermal Systems Design MARYLAND. Fundamentals of heat transfer Radiative equilibrium Surface properties Non-ideal effects

Thermal Systems Design Fundamentals of heat transfer Radiative equilibrium Surface properties Non-ideal effects Internal power generation Environmental temperatures Conduction Thermal system components

Optimization of Thermal Radiation Source for High Temperature Infrared Thermometer Calibration

Optimization of Thermal Radiation Source for High Temperature Infrared Thermometer Calibration Gavin McQuillan NLA T&M Conference Guateng, September 26-28, 2016 2011 Fluke Calibration 1 Outline Introduction

ATMOSPHERIC ENERGY and GLOBAL TEMPERATURES. Physical Geography (Geog. 300) Prof. Hugh Howard American River College

ATMOSPHERIC ENERGY and GLOBAL TEMPERATURES Physical Geography (Geog. 300) Prof. Hugh Howard American River College RADIATION FROM the SUN SOLAR RADIATION Primarily shortwave (UV-SIR) Insolation Incoming

4. Zero-dimensional Model of Earth s Temperature

4. Zero-dimensional Model of Earth s Temperature Introduction The term zero-dimensional implies that the earth is treated as a single point having a single temperature. Later we will consider a one-dimensional

Topics: Visible & Infrared Measurement Principal Radiation and the Planck Function Infrared Radiative Transfer Equation

Review of Remote Sensing Fundamentals Allen Huang Cooperative Institute for Meteorological Satellite Studies Space Science & Engineering Center University of Wisconsin-Madison, USA Topics: Visible & Infrared

Stratospheric Welsbach seeding for reduction of global warming

( 1 of 1 ) United States Patent 5,003,186 Chang, et al. March 26, 1991 Stratospheric Welsbach seeding for reduction of global warming Abstract A method is described for reducing atmospheric or global warming

HEATING THE ATMOSPHERE

HEATING THE ATMOSPHERE Earth and Sun 99.9% of Earth s heat comes from Sun But

Chemistry 795T. Black body Radiation. The wavelength and the frequency. The electromagnetic spectrum. Lecture 7

Chemistry 795T Lecture 7 Electromagnetic Spectrum Black body Radiation NC State University Black body Radiation An ideal emitter of radiation is called a black body. Observation: that peak of the energy

Chapter 1 Blackbody Radiation Experiment objectives: explore radiation from objects at certain temperatures, commonly known as blackbody radiation ; make measurements testing the Stefan-Boltzmann law in

PHYSICS 149: Lecture 26

PHYSICS 149: Lecture 26 Chapter 14: Heat 14.1 Internal Energy 14.2 Heat 14.3 Heat Capacity and Specific Heat 14.5 Phase Transitions 14.6 Thermal Conduction 14.7 Thermal Convection 14.8 Thermal Radiation

= (fundamental constants c 0, h, k ). (1) k

Introductory Physics Laboratory, Faculty of Physics and Geosciences, University of Leipzig W 12e Radiation Thermometers Tasks 1 Measure the black temperature T s of a glowing resistance wire at eight different

Teaching the Greenhouse Effect. Brian Hornbuckle and Ray Arritt

Teaching the Greenhouse Effect Brian Hornbuckle and Ray Arritt It is true that there are other factors (such as volcanic activity, variations in the earth s orbit and axis, the solar cycle), yet a number

Recall: The Importance of Light

Key Concepts: Lecture 19: Light Light: wave-like behavior Light: particle-like behavior Light: Interaction with matter - Kirchoff s Laws The Wave Nature of Electro-Magnetic Radiation Visible light is just

SPH3U1 Lesson 03 Energy

THERMAL ENERGY AND LATENT HEAT LEARNING GOALS Students will learn: Heat changes the amount of thermal energy in an object Temperature is a measure of the average thermal energy in an object Heat capacity

Habitable Planets. Much of it stolen from. Yutaka ABE University of Tokyo

Habitable Planets Much of it stolen from Yutaka ABE University of Tokyo 1. Habitability and Water Why water? Importance of Liquid Gas: highly mobile, but low material density. Solid: high density but very

Chapter 11. Energy in Thermal Processes

Chapter 11 Energy in Thermal Processes Vocabulary, 3 Kinds of Energy Internal Energy U = Energy of microscopic motion and intermolucular forces Work W = -F x = -P V is work done by compression (next chapter)

Project 3 Convection and Atmospheric Thermodynamics

12.818 Project 3 Convection and Atmospheric Thermodynamics Lodovica Illari 1 Background The Earth is bathed in radiation from the Sun whose intensity peaks in the visible. In order to maintain energy balance

Lecture 3: Emission and absorption

Lecture 3: Emission and absorption Senior Astrophysics 2017-03-10 Senior Astrophysics Lecture 3: Emission and absorption 2017-03-10 1 / 35 Outline 1 Optical depth 2 Sources of radiation 3 Blackbody radiation

Earth! Objectives: Interior and plate tectonics Atmosphere and greenhouse effect

Earth! Objectives: Interior and plate tectonics Atmosphere and greenhouse effect Earth Fun Facts 1. Only body with liquid water on the surface. 2. Most massive terrestrial body in solar system 3. Only

Clouds and Rain Unit (3 pts)

Name: Section: Clouds and Rain Unit (Topic 8A-2) page 1 Clouds and Rain Unit (3 pts) As air rises, it cools due to the reduction in atmospheric pressure Air mainly consists of oxygen molecules and nitrogen

THE GREENHOUSE EFFECT

ASTRONOMY READER THE GREENHOUSE EFFECT 35.1 THE GREENHOUSE EFFECT Overview Planets are heated by light from the Sun. Planets cool off by giving off an invisible kind of light, longwave infrared light.

Lecture Outlines PowerPoint. Chapter 16 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint Chapter 16 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

!U = Q " P!V. Q = mc!t. Vocabulary, 3 Kinds of Energy. Chapter 11. Energy in Thermal Processes. Example Temperature and Specific Heat

Vocabulary, 3 Kinds of Energy Chapter 11 Energy in Thermal Processes Internal Energy U = Energy of microscopic motion and intermolucular forces Work W = -F!x = -P!V is work done by compression (next chapter)

M13/4/PHYSI/HPM/ENG/TZ1/XX. Physics Higher level Paper 1. Monday 6 May 2013 (morning) 1 hour INSTRUCTIONS TO CANDIDATES

M13/4/PHYSI/HPM/ENG/TZ1/XX 22136507 Physics Higher level Paper 1 Monday 6 May 2013 (morning) 1 hour INSTRUCTIONS TO CANDIDATES Do not open this examination paper until instructed to do so. Answer all the

Chapter 11 The Formation of Stars

Chapter 11 The Formation of Stars A World of Dust The space between the stars is not completely empty, but filled with very dilute gas and dust, producing some of the most beautiful objects in the sky.

AT 350 EXAM #1 February 21, 2008

This exam covers Ahrens Chapters 1 and 2, plus related lecture notes Write the letter of the choice that best completes the statement or answers the question. b_ 1. The Earth s atmosphere is currently

Introduction and Fundamental Concepts

Chapter1 Introduction and Fundamental Concepts CHAPTER OUTLINE 1.1 Heat Transfer Fundamentals 2 1.1.1 Conduction 3 1.1.2 Convection 4 1.1.3 Radiation 6 1.1.3.1 Blackbody Radiation 6 1.2 Entropy Flow and

exp ( κh/ cos θ) whereas as that of the diffuse source is never zero (expect as h ).

Homework 3: Due Feb 4 1. 2.11 Solution done in class 2. 2.8 The transmissivity along any dection is exp ( κh/ cos θ) where h is the slab thickness and θ is the angle between that dection and the normal

Thermal Conductivity, k

Homework # 85 Specific Heats at 20 C and 1 atm (Constant Pressure) Substance Specific Heat, c Substance Specific Heat, c kcal/kg C J/kg C kcal/kg C J/kg C Solids Aluminum 0.22 900 Brass 0.090 377 Copper

Shape and Size of the Earth

Planet Earth Shape and Size of the Earth Gravity is what gives Earth its spherical shape Only effective if the body is of a critical size Critical radius is about 350 km Shape and Size of the Earth Earth

Key Concept Heat in Earth s atmosphere is transferred by radiation, conduction, and convection.

Section 2 Atmospheric Heating Key Concept Heat in Earth s atmosphere is transferred by radiation, conduction, and convection. What You Will Learn Solar energy travels through space as radiation and passes

Name Class Date. What are three kinds of energy transfer? What are conductors and insulators? What makes something a good conductor of heat?

CHAPTER 14 SECTION Heat and Temperature 2 Energy Transfer KEY IDEAS As you read this section, keep these questions in mind: What are three kinds of energy transfer? What are conductors and insulators?

FOLLOW THE ENERGY! EARTH S DYNAMIC CLIMATE SYSTEM

Investigation 1B FOLLOW THE ENERGY! EARTH S DYNAMIC CLIMATE SYSTEM Driving Question How does energy enter, flow through, and exit Earth s climate system? Educational Outcomes To consider Earth s climate

Chapter 11. Energy in Thermal Processes

Chapter 11 Energy in Thermal Processes Vocabulary, 3 Kinds of Energy Internal Energy U Energy of a system due to microscopic motion and inter-molucular forces Work W -F x -P V is work done by expansion

Chapter 17. Work, Heat, and the First Law of Thermodynamics Topics: Chapter Goal: Conservation of Energy Work in Ideal-Gas Processes

Chapter 17. Work, Heat, and the First Law of Thermodynamics This false-color thermal image (an infrared photo) shows where heat energy is escaping from a house. In this chapter we investigate the connection

Name: Partner(s): 1102 or 3311: Desk # Date: Spectroscopy Part I

Name: Partner(s): 1102 or 3311: Desk # Date: Spectroscopy Part I Purpose Investigate Kirchhoff s Laws for continuous, emission and absorption spectra Analyze the solar spectrum and identify unknown lines

Intro to Galaxies Light and Atoms - I

Astrophysics Study of Light Study of Atoms Intro to Galaxies Light and Atoms - I 1 Atomic Physics elements: substances which cannot be broken down into simpler substances atom : smallest unit of an element

The Sun: Our Star. The Sun is an ordinary star and shines the same way other stars do.

The Sun: Our Star The Sun is an ordinary star and shines the same way other stars do. Announcements q Homework # 4 is due today! q Units 49 and 51 Assigned Reading Today s Goals q Today we start section

The Basics of Light. Sunrise from the Space Shuttle, STS-47 mission. The Basics of Light

The Basics of Light The sun as it appears in X-ray light (left) and extreme ultraviolet light (right). Light as energy Light is remarkable. It is something we take for granted every day, but it's not something

The Sun. Chapter 12. Properties of the Sun. Properties of the Sun. The Structure of the Sun. Properties of the Sun.

Chapter 12 The Sun, Our Star 1 With a radius 100 and a mass of 300,000 that of Earth, the Sun must expend a large amount of energy to withstand its own gravitational desire to collapse To understand this

Pre-Lab Reading Questions GS106 Lab 3 Answer Key - How We Use Light in Astronomy Life Cycle of a Wave: 1) initialized as oscillating vibrations ("disturbances"), 2) wave travel from origin to destination,

The Night Sky. The Universe. The Celestial Sphere. Stars. Chapter 14

The Night Sky The Universe Chapter 14 Homework: All the multiple choice questions in Applying the Concepts and Group A questions in Parallel Exercises. Celestial observation dates to ancient civilizations

Atoms and Star Formation

Atoms and Star Formation What are the characteristics of an atom? Atoms have a nucleus of protons and neutrons about which electrons orbit. neutrons protons electrons 0 charge +1 charge 1 charge 1.67 x

Infrared Spectroscopy: Identification of Unknown Substances

Infrared Spectroscopy: Identification of Unknown Substances Suppose a white powder is one of the four following molecules. How can they be differentiated? H N N H H H H Na H H H H H A technique that is