Milne–Eddington approximation

E818289

The Milne–Eddington approximation is a simplified model of stellar atmospheres that assumes constant physical properties with depth to make the radiative transfer equations analytically tractable.

All labels observed (3)

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Statements (48)

Predicate Object
instanceOf astrophysical approximation ⓘ
radiative transfer model ⓘ
stellar atmosphere model ⓘ
advantage analytic tractability ⓘ
computational simplicity ⓘ
appliesTo stellar atmospheres ⓘ
approximationOf full depth-dependent radiative transfer solution ⓘ
assumes constant continuum opacity with depth ⓘ
constant line absorption coefficient with depth ⓘ
constant physical properties with depth ⓘ
gray atmosphere in many applications ⓘ
linear source function with optical depth ⓘ
local thermodynamic equilibrium ⓘ
plane-parallel atmosphere ⓘ
static atmosphere ⓘ
basedOn Eddington approximation ⓘ
characteristic allows closed-form expressions for emergent intensity ⓘ
allows closed-form expressions for emergent polarization ⓘ
neglects depth variation of many atmospheric parameters ⓘ
treats line and continuum opacities in a simplified way ⓘ
comparedTo more realistic multi-layer atmosphere models ⓘ
field astrophysics ⓘ
radiative transfer theory ⓘ
stellar astrophysics ⓘ
historicalContext developed in early 20th century ⓘ
involves constant line-to-continuum opacity ratio ⓘ
solution of the radiative transfer equation for a two-level atom in simplified form ⓘ
source function linear in optical depth ⓘ
limitation cannot accurately represent strongly stratified atmospheres ⓘ
limited accuracy for lines formed over large height ranges ⓘ
namedAfter Arthur Stanley Eddington ⓘ
Edward Arthur Milne ⓘ
purpose to interpret solar spectra ⓘ
to interpret stellar spectra ⓘ
to model spectral line formation ⓘ
to obtain analytic solutions for radiative transfer ⓘ
to simplify the radiative transfer equation ⓘ
relatedTo polarized radiative transfer ⓘ
radiative transfer equation ⓘ
spectral line formation theory ⓘ
stellar atmosphere theory ⓘ
typicalApplication quick inversion of large spectropolarimetric data sets ⓘ
solar photospheric line modeling ⓘ
usedFor analytic treatment of polarized radiative transfer ⓘ
inversion of spectropolarimetric data ⓘ
magnetic field diagnostics in stellar atmospheres ⓘ
modeling of Stokes profiles ⓘ
solar magnetic field measurements ⓘ

How these facts were elicited

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

Edward Arthur Milne → hasConceptNamedAfter → Milne–Eddington approximation ⓘ
Eddington standard model of stars → uses → Eddington approximation for radiative transfer ⓘ
linked to: Milne–Eddington approximation
Schuster–Schwarzschild theorem → relatedTo → Milne–Eddington atmosphere ⓘ
linked to: Milne–Eddington approximation