Oppgavesett kap. 4 (1 av 2) GEF2200

Similar documents
Radiation in the atmosphere

Radiative Equilibrium Models. Solar radiation reflected by the earth back to space. Solar radiation absorbed by the earth

Lecture 2 Global and Zonal-mean Energy Balance

What is it good for? RT is a key part of remote sensing and climate modeling.

Spectrum of Radiation. Importance of Radiation Transfer. Radiation Intensity and Wavelength. Lecture 3: Atmospheric Radiative Transfer and Climate

Lecture 3: Atmospheric Radiative Transfer and Climate

Blackbody radiation. Main Laws. Brightness temperature. 1. Concepts of a blackbody and thermodynamical equilibrium.

Solar radiation / radiative transfer

1. Radiative Transfer. 2. Spectrum of Radiation. 3. Definitions

Radiation and the atmosphere

Description of radiation field

Lecture 4: Radiation Transfer

1. Weather and climate.

MASSACHUSETTS INSTITUTE OF TECHNOLOGY Department of Physics Problem Solving 10: The Greenhouse Effect. Section Table and Group

Lecture 5: Greenhouse Effect

Take away concepts. What is Energy? Solar Radiation Emission and Absorption. Energy: The ability to do work

Fundamentals of Atmospheric Radiation and its Parameterization

Lecture 5: Greenhouse Effect

Blackbody Radiation. A substance that absorbs all incident wavelengths completely is called a blackbody.

Monday 9 September, :30-11:30 Class#03

Which picture shows the larger flux of blue circles?

Radiation from planets

Lecture 4: Global Energy Balance

Lecture 4: Global Energy Balance. Global Energy Balance. Solar Flux and Flux Density. Blackbody Radiation Layer Model.

Lecture 2: principles of electromagnetic radiation

ATMOS 5140 Lecture 7 Chapter 6

Questions you should be able to answer after reading the material

Earth: A Dynamic Planet A. Solar and terrestrial radiation

Advanced Heat and Mass Transfer by Amir Faghri, Yuwen Zhang, and John R. Howell

Chapter 3 Energy Balance and Temperature. Astro 9601

2. Illustration of Atmospheric Greenhouse Effect with Simple Models

E d. h, c o, k are all parameters from quantum physics. We need not worry about their precise definition here.

Chapter 3 Energy Balance and Temperature. Topics to be covered

Preface to the Second Edition. Preface to the First Edition

Goal: The theory behind the electromagnetic radiation in remote sensing. 2.1 Maxwell Equations and Electromagnetic Waves

Lecture 4: Heat, and Radiation

MAPH & & & & & & 02 LECTURE

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

P607 Climate and Energy (Dr. H. Coe)

With certain caveats (described later) an object absorbs as effectively as it emits

Modeling of Environmental Systems

INTRODUCTION Radiation differs from conduction and convection in that it does not require the presence of a material medium to take place.

Lecture 2: Global Energy Cycle

Sources of radiation

ME 476 Solar Energy UNIT TWO THERMAL RADIATION

Radiation in the Earth's Atmosphere. Part 1: Absorption and Emission by Atmospheric Gases

8.5 GREENHOUSE EFFECT 8.6 GLOBAL WARMING HW/Study Packet

- matter-energy interactions. - global radiation balance. Further Reading: Chapter 04 of the text book. Outline. - shortwave radiation balance

Lecture 3: Global Energy Cycle

ASTR240: Radio Astronomy

Atmospheric Radiation

Tananyag fejlesztés idegen nyelven

Physical Basics of Remote-Sensing with Satellites

Temperature Scales

Numerical Heat and Mass Transfer

Energy and Radiation. GEOG/ENST 2331 Lecture 3 Ahrens: Chapter 2

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

Chemistry 795T. Lecture 7. Electromagnetic Spectrum Black body Radiation. NC State University

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

Solar radiation - the major source of energy for almost all environmental flows

Lecture Notes Prepared by Mike Foster Spring 2007

Lecture Outline. Energy 9/25/12

M.Sc. in Meteorology. Physical Meteorology Prof Peter Lynch. Mathematical Computation Laboratory Dept. of Maths. Physics, UCD, Belfield.

Global Energy Balance. GEOG/ENST 2331: Lecture 4 Ahrens: Chapter 2

Energy. Kinetic and Potential Energy. Kinetic Energy. Kinetic energy the energy of motion

Hand in Question sheets with answer booklets Calculators allowed Mobile telephones or other devices not allowed

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

1. SOLAR GEOMETRY, EXTRATERRESTRIAL IRRADIANCE & INCIDENCE ANGLES

Monday, Oct. 2: Clear-sky radiation; solar attenuation, Thermal. nomenclature

Fundamental Concepts of Radiation -Basic Principles and Definitions- Chapter 12 Sections 12.1 through 12.3

Lecture # 04 January 27, 2010, Wednesday Energy & Radiation

Chemistry 431. Lecture 1. Introduction Statistical Averaging Electromagnetic Spectrum Black body Radiation. NC State University

Torben Königk Rossby Centre/ SMHI

Lecture 3: Emission and absorption

Emission Temperature of Planets. Emission Temperature of Earth

Earth: the Goldilocks Planet

Introduction to Electromagnetic Radiation and Radiative Transfer

AT622 Section 3 Basic Laws

ATMO/OPTI 656b Spring 2009

THE EXOSPHERIC HEAT BUDGET

Thursday, November 1st.

Name(s) Period Date. Earth s Energy Budget: How Is the Temperature of Earth Controlled?

Radiative Balance and the Faint Young Sun Paradox

Earth s Energy Budget: How Is the Temperature of Earth Controlled?

The Stefan-Boltzmann law is an example of a power law.

Electromagnetic Radiation. Radiation and the Planetary Energy Balance. Electromagnetic Spectrum of the Sun

2. Energy Balance. 1. All substances radiate unless their temperature is at absolute zero (0 K). Gases radiate at specific frequencies, while solids

point, corresponding to the area it cuts out: θ = (arc length s) / (radius of the circle r) in radians Babylonians:

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

ATM 507 Lecture 4. Text reading Chapters 3 and 4 Today s topics Chemistry, Radiation and Photochemistry review. Problem Set 1: due Sept.

Beer-Lambert (cont.)

Thermal Radiation By: Prof. K M Joshi

Radiative Transfer Multiple scattering: two stream approach 2

9/5/16. Section 3-4: Radiation, Energy, Climate. Common Forms of Energy Transfer in Climate. Electromagnetic radiation.

Understanding the Greenhouse Effect

Radiation in climate models.

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

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

12.815/12.816: RADIATIVE TRANSFER PROBLEM SET #1 SOLUTIONS

Earth Systems Science Chapter 3

Transcription:

Oppgavesett kap. 4 (1 av 2) GEF2200 hans.brenna@geo.uio.no Exercise 1: Wavelengths and wavenumbers (We will NOT go through this in the group session) What's the relation between wavelength and wavenumber? Figure 1 shows emssion spectra from two dierent bodies. Spectrum A in Figure 1a shows emitted intensity as a function of wavelength, λ, while spectrym B in Figure 1b shows emitted intensity as a function of wavenumber, ν. Look at the x-axis in Figure 1a. Is more energetic, short wave radiation towards the left or right of the spectrum? Look at the x-axis in Figure 1b. Is more energetic, short wave radiation towards the left or right of the spectrum? e) The spectrum in Figure 1a illustrates the radtiation intensity of the Sun, while the spectrum in Figure 1b illustrates the radiation intensity of the Earth (Both simplied). It's common to use wavelength in µm as the x-axis for the solar spectrum and wavenumber in cm 1 as the x-axis for the terrestrial spectrum. Why do you think it's like this? (Hint: See gure 4.6 in W&H) 1

( Spectrum A ( Spectrum B Figure 1: Emission spectra from two dierent bodies d) Which types of radiation do the Sun and Earth emit most intensely? Exercise 2: Radiance og irradiance What is a solid angle? Dene the following quantities and specify their corresponding units: 2

ˆ Monochromatic intensity (monochromatic radiance). ˆ Intensity (radiance). ˆ Monochromatic ux density (monochromatic irradiance). ˆ Flux density (irradiance). Consider Figure 4.3 in W&H and show that a small change in solid angle ω is given as dω = sin θdθdφ d) Exercise 4.14 in W&H e) What does isotropic radiation mean? f) A measuring station which measures monochromatic ux density, F λ is located in an area with mountains on all sides so the horizon is not located at zenith angle 90, but at 80 (see Figure 2). This means the sky does not span a solid angle of 2π as shown in example 4.1 in W&H, but a little less. The station is exposed to isotropic, monochromatic intensity, I λ. Calculate the monochromatic ux density F λ recieved at the station. Figure 2: Measuring station surrounded by mountains on all sides. 3

g) Radiation is emitted by a body. How has the intesity and ux density changed when we are at a distance d away from the body? Use the inverse square law in your explanation. Oppgave 3: Sortlegemestråling (fra eksamen 2007) What is a black body? Which of these can be approximated as a black body: ˆ The Earth ˆ The Sun ˆ The atmosphere Write down the following laws/functions and explain briey what thei describe and the mathematic relations between them: ˆ Plancks function ˆ Wiens law ˆ Stefan Boltzmanns law The fux density of solar radiation incident on the top of the Earth's atmosphere is given by the solar constant F s = 1368 Wm 2. The earth's radius is R E = 6, 371 10 6 m. 1. How much energy does the Earth recieve from the Sun every second? Neglect the Earth's albedo. 2. How large must the irradiance of the Earth be to achieve radiative equilibrium with the recieved energy you calculated abovet? (Again neglecting the Earth's albedo) 3. The black body temperature of the Earth is -18 C. Show that the planetary albedo is 0.3. 4

4. How can the mean temperature at the Earth's surface be 15 C, when the black body temperature is -18 C? Exercise 4 Dene the terms monochomatic... ˆ emissivity ˆ absorptivity ˆ reectivity ˆ transmissivity Exercise 4.15 A non-black body (A) is assumed to emits radiation with the same emissivity for every wavelength. We assume the body emits the same irradiance/ux density, F, as a black body (B). Which of the two bodies (A or B) has the highets temperature? Explain your answer. d) The incident radiation at the top of a non-reective, absorbing atmospheric layer is I λ,1 = 5 Wm 2 µm 1 sr 1. I λ,2 = 3 Wm 2 µm 1 sr 1 is transmitted through the layer. What is the transmissivity (T λ ) og absorptivity (α λ ) of the layer? e) What is Kirchhos law, and when does it apply? 5

Exercise 5 Blue light with wavelength λ = 0, 5 µm is scattered bu air molecules with radiuss 10 4 µm. 1. Which type of scattering is this? 2. Which of the gures in Figure 4.12 in W&H best corresponds to this type of scattering? 3. How does the scattering eciency K λ change with wavelength in this scattering regime? Explain the following: ˆ Blue sky ˆ Red sunsets Oppgave 6 What is broadening, and why is this interesting with regards to climate change? Which types of broadening do we have and in which parts of the atmosphere does the dierent types dominate? 6