Gray Case1 The Gray Case Let us assume that the opacity is independent of frequency: Κ ν → Κ NB: This does not mean I ν = I, that is, the intensity (flux,

Slides:



Advertisements
Similar presentations
Stellar Structure Section 4: Structure of Stars Lecture 8 – Mixing length theory The three temperature gradients Estimate of energy carried by convection.
Advertisements

Transient Conduction: The Lumped Capacitance Method
Nuclear Astrophysics Lecture 5 Thurs. Nov. 21, 2011 Prof. Shawn Bishop, Office 2013, Ex
Nuclear Astrophysics Lecture 4 Thurs. Nov. 11, 2011 Prof. Shawn Bishop, Office 2013, Extension
Stellar Atmospheres: Hydrostatic Equilibrium 1 Hydrostatic Equilibrium Particle conservation.
Chapter 16 – Vector Calculus 16.7 Surface Integrals 1 Objectives:  Understand integration of different types of surfaces Dr. Erickson.
Lesson 3 METO 621. Basic state variables and the Radiative Transfer Equation In this course we are mostly concerned with the flow of radiative energy.
Radiative Equilibrium. Radaitive Equilibrium2 The Condition of Radiative Equilibrium Modes of Energy Transport Modes of Energy Transport Radiative Radiative.
Sub-THz Component of Large Solar Flares Emily Ulanski December 9, 2008 Plasma Physics and Magnetohydrodynamics.
Department of Physics National Tsing Hua University G.T. Chen 2005/11/3 Model Spectra of Neutron Star Surface Thermal Emission ---Diffusion Approximation.
METO 621 Lesson 9. Solution for Zero Scattering If there is no scattering, e.g. in the thermal infrared, then the equation becomes This equation can be.
Astro 300B: Jan. 24, 2011 Optical Depth Eddington Luminosity Thermal radiation and Thermal Equilibrium.
METO 621 LESSON 8. Thermal emission from a surface Let be the emitted energy from a flat surface of temperature T s, within the solid angle d  in the.
METO 621 Lesson 13. Separation of the radiation field into orders of scattering If the source function is known then we may integrate the radiative transfer.
METO 621 Lesson 19. Role of radiation in Climate We will focus on the radiative aspects of climate and climate change We will use a globally averaged.
METO 621 Lesson 10. Upper half-range intensity For the upper half-range intensity we use the integrating factor e -  In this case we are dealing with.
Physics 681: Solar Physics and Instrumentation – Lecture 4
Model Spectra of Neutron Star Surface Thermal Emission Department of Physics National Tsing Hua University Lun-Wen Yeh
Model spectra of neutron star surface thermal emission soccer
Model Spectra of Neutron Star Surface Thermal Emission Soccer
Model Spectra of Neutron Star Surface Thermal Emission Department of Physics National Tsing Hua University Lun-Wen Yeh
Feb. 2, 2011 Rosseland Mean Absorption Poynting Vector Plane EM Waves The Radiation Spectrum: Fourier Transforms.
Transient Conduction: The Lumped Capacitance Method
Interesting News… Regulus Age: a few hundred million years Mass: 3.5 solar masses Rotation Period:
Ch. 5 - Basic Definitions Specific intensity/mean intensity Flux
Stellar Atmospheres: The Radiation Field 1 The Radiation Field.
Radiation Definitions and laws Heat transfer by conduction and convection required the existence of a material medium, either a solid or a.
Section 5: The Ideal Gas Law The atmospheres of planets (and the Sun too) can be modelled as an Ideal Gas – i.e. consisting of point-like particles (atoms.
Now we begin…..
Basic Definitions Terms we will need to discuss radiative transfer.
Rotation of Regulus Age: a few hundred million years
Review of Lecture 4 Forms of the radiative transfer equation Conditions of radiative equilibrium Gray atmospheres –Eddington Approximation Limb darkening.
Stellar Atmospheres II
Stellar structure equations
Radiative Equilibrium
Ch. 5 - Basic Definitions Specific intensity/mean intensity Flux
Stellar Atmospheres: Radiation Transfer 1 Radiation Transfer.
Lecture 3 Radiative and Convective Energy Transport I.Mechanisms of Energy Transport II. Radiative Transfer Equation III. Grey Atmospheres IV. Convective.
Space Science : Atmosphere Part-5 Planck Radiation Law Local Thermodynamic Equilibrium: LET Radiative Transport Approximate Solution in Grey Atmosphere.
Radiation Fundamental Concepts EGR 4345 Heat Transfer.
Energy Transport Formal solution of the transfer equation Radiative equilibrium The gray atmosphere Limb darkening.
CBE 150A – Transport Spring Semester 2014 Radiation.
1 The structure and evolution of stars Lecture 3: The equations of stellar structure.
1 Grey Atmosphere (Mihalas 3) Eddington Approximation Solution Temperature Stratification Limb Darkening Law Λ-iteration, Unsőld iteration Method of Discrete.
A540 Review - Chapters 1, 5-10 Basic physics Boltzman equation
Firohman Current is a flux quantity and is defined as: Current density, J, measured in Amps/m 2, yields current in Amps when it is integrated.
M.R. Burleigh 2601/Unit 4 DEPARTMENT OF PHYSICS AND ASTRONOMY LIFECYCLES OF STARS Option 2601.
1 Analytical Relations for the Transfer Equation (Mihalas 2) Formal Solutions for I, J, H, K Moments of the TE w.r.t. Angle Diffusion Approximation.
1 Model Atmosphere Results (Kurucz 1979, ApJS, 40, 1) Kurucz ATLAS LTE code Line Blanketing Models, Spectra Observational Diagnostics.
Lecture 8 Radiative transfer.
Hale COLLAGE (CU ASTR-7500) “Topics in Solar Observation Techniques” Lecture 2: Describing the radiation field Spring 2016, Part 1 of 3: Off-limb coronagraphy.
1 ASTR 8000 STELLAR ATMOSPHERES AND SPECTROSCOPY Introduction & Syllabus Light and Matter Sample Atmosphere.
Spectral Line Transfer Hubeny & Mihalas Chap. 8 Mihalas Chap. 10 Definitions Equation of Transfer No Scattering Solution Milne-Eddington Model Scattering.
1 Equation of Transfer (Mihalas Chapter 2) Interaction of Radiation & Matter Transfer Equation Formal Solution Eddington-Barbier Relation: Limb Darkening.
Basic Definitions Specific intensity/mean intensity Flux
Chapter 9 Stellar Atmospheres. Specific Intensity, I I ( or I ) is a vector (units: W m -2 Hz -1 sterad -1 )
Lecture 8: Stellar Atmosphere 4. Stellar structure equations.
Heat Transfer RADIATION HEAT TRANSFER FUNDAMENTALS.
Lecture 8: Stellar Atmosphere 3. Radiative transfer.
Lecture 8: Stellar Atmosphere
The Transfer Equation The basic equation of transfer for radiation passing through gas: the change in specific intensity In is equal to: dIl = intensity.
Lesson 1: Prerequisites
Grey Atmosphere (Hubeny & Mihalas 17, 13)
Lesson 1: Prerequisites
Numerical Model Atmospheres (Hubeny & Mihalas 16, 17)
Lesson 1: Prerequisites
Analytical Relations for the Transfer Equation (Hubeny & Mihalas 11)
Terms we will need to discuss radiative transfer.
Grey Atmosphere (Hubeny & Mihalas 17, 13)
Equation of Transfer (Hubeny & Mihalas Chapter 11)
Presentation transcript:

Gray Case1 The Gray Case Let us assume that the opacity is independent of frequency: Κ ν → Κ NB: This does not mean I ν = I, that is, the intensity (flux, etc) ARE frequency dependent.

Gray Case2 Equation of Transfer Assume Radiative equilibrium

Gray Case3 Continuing: Assume LTE ==> S ν = B ν ==> J(τ) = S(τ) = B(τ) But B(τ) = σT 4 /π Remember:

Gray Case4 On We Go... Now Integrate over all solid angles:

Gray Case5 More Equations! Multiply by μdω/4π (i.e.. Take the 1 st moment) Note: Therefore:

Gray Case6 Make An Assumption! To proceed further (to this point we have been rather rigorous (e.g., we assume LTE and radiative equilibrium but do everything else properly). In the interior of a star I ≠ f(θ) so consider K = 1/4π ∫I(θ) cos 2 θdω But if I ≠ f(θ) then

Gray Case7 What About J? If I ≠ f(θ) then J = I/4π∫dω = I but this means K → J / 3 Here’s the approximation: K = J/3 everywhere. This is called the Eddington Approximation. dK/dτ = H dJ/dτ = 3H or J = 3Hτ + C Now Let us Consider the Intensities

Gray Case8 Gray Case Intensity We will consider that I ≠ f(θ) except for the general distinction between an inward and an outward flow: I(θ) = I 1 : 0 < θ < π/2 Outward = I 2 : π/2 < θ < π Inward We shall also assume that at the surface that I is constant over the hemisphere and that there is no inward flux (I 2 = 0) so

Gray Case9 Continuing On.... What we want is the constant is the constant in J = 3Hτ + C At the Surface I 2 = 0 so J 0 = I 0 /2 H 0 = I 0 /4 which means H 0 = J 0 /2 So J = 3Hτ + C evaluated at τ=0 (the surface) yields: 2H = C  J(τ) = 3Hτ + 2H = H(3τ + 2) But note that F A = 4H so J(τ) = (F/4)(3τ + 2)

Gray Case10 The T - τ Relation A Relation of Fundamental Importance is the relation between the temperature T and the optical depth τ. For the Gray Case: J(τ) = H(3τ + 2) But in LTE: J = B  B(T) = H(3τ + 2) But this is the Integrated B = σT 4 /π so σT 4 /π = H(3τ + 2)

Gray Case11 More on T-τ At τ 0 = 0 we have σT 0 4 /π = 2H so σT 4 /π = 3Hτ + 2H = σT 0 4 /π + 3/2 σT 0 4 /π τ T 4 = T /2 T 0 4 τ = T 0 4 (1 + 3/2 τ) But what is T 0 ? Well remember that F P =4πH = σT 4 and F A = 4H = σT 4 /π The definition of T eff is F P = σT eff 4 2H = σT eff 4 /2π = σT 0 4 /π

Gray Case12 The T-τ Relation For the Sun T eff = 5740 K which yields T 0 = 4826 K so to specify the temperature structure T 4 = 1/2 T eff 4 (1 + 3/2 τ) NB: T = T eff at τ = 2/3