2.6 Flashcards

1
Q

Approximation for 1-dimensional, or plane-parallel atmosphere

(radiative transfer for)

A
  • Temperature T constant for horizontal plane
  • structure varies only in vertical direction z
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2
Q

Path d s in a plane-parallel atmosphere

A

ds = dz / cos(θ) = dz / μ

  • μ = cos(θ)
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3
Q

Radiative transfer equation for a plane-parallel atmosphere

A

μ ∂Iν(z, μ) / ∂z = jν - αν Iν

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4
Q

Definition of optical depth τ

A

ν = -αν dz

  • optical depth τν(z) as function of vertical distance z
  • τν = 0 at top of atmosphere
  • τν increases with increasing depth or decreasing height
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5
Q

Radiative transfer equation as a function of τν(z)

A

μ ∂Iνν, ν) / ∂τν = Iν - Sν

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6
Q

Solution of radiative transfer equation

not what it is but how it is obtained

for a plane-parallel stellar atmosphere

A

Obtained by multiplying with eν / μ and integrating from a reference optical depth τν,0

some additional context might be good if this is relevant

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7
Q

Case I: Outward ray

radiative transfer as a function of optical depth

A
  • 0 ≤ μ ≤ 1, cos(theta) positive
  • ray starts very deep at τν,0 = ∞
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8
Q

Case II: Inward ray

Add Clarifier

A

0 ≥ μ ≥ -1, inward ray from surface τν,0 = 0

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9
Q

Important approximation for intensity I(τν, μ)

A

If τν » 1:

Iνν, μ) = Bνν) + μ dBνν) / dτν

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10
Q

Anisotropic part of radiation field

A

- μ · dBν / dτν,

  • negative for inward direction
  • positive for outward direction
  • zero parallel to surface

so the first line is in fact the anis. part but the following seems to refer to mu = cos theta. im not sure if thats also called the anis. part. Also i am not sure what inward and outward are referring to here

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11
Q

Radiation parameters U𝛎, F𝛎, P𝛎 for plane-parallel atmosphere

A
  • Energy density
  • Flux
  • Radiation pressure calculated using function A(cos θ)

not sure what the calculated using … is about

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12
Q

Ratio between anisotropic and isotropic parts of the radiation field

A

(dBν / dτν) / Bν ≈ 3Fν / cUν

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13
Q

Integration over all wavelengths for anisotropic and isotropic terms

A

Anisotropic term / Isotropic term ≈ 3F / cU

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14
Q

Energy density U for blackbody radiation

formula

A

U = aT4(τ),
where a = 4σ / c

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15
Q

Total flux F emerging from surface with effective temperature Teff

A

F = σTeff4

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16
Q

Anisotropy expressed in temperatures

A

Anisotropic term / Isotropic term ≈ 3/4 (Teff / T(τ))4