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Atmospheres of Cool Stars

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Title: Atmospheres of Cool Stars


1
Atmospheres of Cool Stars
  • Radiative Equilibrium ModelsExtended
    AtmospheresHeating Theories

2
Radiative Equilibrium Models
  • Gustafson et al. (2005) MARCS codedifficult
    because of UV line haze(millions of b-b
    transitions of Fe I in 300-400 nm range, and Fe
    II in 200-300 nm range)
  • Convection important at depth
  • Metallicity and line blanketing causes surface
    cooling and back warming

3
Dwarfs Giants
  • Solid line Solar abundancesFe/H0
  • Dashed line Metal poorFe/H-2
  • Dot-dashed Kurucz LTE-RE model

4
Semi-empirical Models Based on Observations of
I?(µ1,t1)
  • Solar spectrum shows non-thermal components at
    very long and short wavelengths that indicate
    importance of other energy transport mechanisms

5
  • Major b-b and b-f transitions for solar opacity
    changes

6
  • Determine central specific intensity across
    spectrum
  • Get brightness temperaturefrom Planck curve for
    I?
  • From opacity get optical depth on standard depth
    scale
  • T(h) for hheight

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9
Reality Structured and Heated
Opticalphotosphere
EUV higher
X-ray higher yet
10
Extended Atmospheres
  • Photosphere
  • Chromosphere
  • Transition region
  • Corona
  • Wind

11
Corona
  • Observed during solar eclipses or by coronagraph
    (electron scattering in optical)
  • Nearly symmetric at sunspot maximum,
    equatorially elongated at sunspot minimum
  • Structure seen in X-rays (no X-ray emission from
    cooler, lower layers)
  • Coronal lines identified by Grotrian, Edlén
    (1939) Fe XIV 5303, Fe X 6374, Ca XV 5694
  • High ionization level and X-rays indicate T106 K

12
X-ray image of Suns hot coronal gas
13
Chromosphere
  • Named for bright colors (flash spectrum)
    observed just before and after total eclipse
  • H Balmer, Fe II, Cr II, Si II lines present
    indicates T 6000 10000 K
  • Lines from chromosphere appear in UV (em. for
    ?lt1700 Å absorption for ?gt1700 Å)
  • Large continuous opacity in UV, but lines have
    even higher opacity appear in emission when
    temperature increases with height

14
Transition Region
  • Seen in high energy transitions which generally
    require large energies (usually in lines with
    ?lt2000 Å)
  • Examples in solar spectrumSi IV 1400, C IV 1550
    (resonance or ground state transitions)

15
Stellar Observations
  • Chromospheric and transition region lines seen in
    UV spectra of many F, G, K-type stars
    (International Ultraviolet Explorer)
  • O I 1304, C I 1657, Mg II 2800
  • Ca II 3968, 3933 (H, K) lines observed as
    emission in center of broad absorption (related
    to sunspot number in Sun useful for starspots
    and rotation in other stars)
  • Emission declines with age (rotation)

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18
Chromospheres in H-R Diagram
  • Emission lines appear in stars found cooler than
    Cepheid instability strip
  • Red edge of strip formed by onset of significant
    convection that dampens pulsations
  • Suggests heating is related to mechanical motions
    in convection

19
Coronae in H-R Diagram
  • Upper luminosity limit for stars with transition
    region lines and X-ray coronal emission
  • Heating not effective in supergiants (but mass
    loss seen)

20
Theory of Atmospheric Heating
  • Increase in temperature cannot be due to
    radiative or thermal processes
  • Need heating by mechanical or magneto-electrical
    processes

21
Acoustic Heating
  • Large turbulent velocities in solar granulation
    are sources of acoustic (sound) waves
  • Lightman (1951), Proudman (1952) show that energy
    flux associated with waves iswhere v
    turbulent velocity and cs speed of sound

22
Acoustic Heating
  • Acoustic waves travel upwards with energy flux
    (energy density) x (propagation speed) ½ ? v2
    cs
  • If they do not lose energy, then speed must
    increase as density decreases? form shock waves
    that transfer energy into the surrounding gas

23
Wave Heating
  • In presence of magnetic fields, sound and shock
    waves are modified into magneto-hydrodynamic
    (MHD) waves of different kinds
  • Damping (energy loss) of acoustic modes depends
    on wave periodex. 5 minute oscillations of Sun
    in chromosphere with T 10000 K yields a damping
    length of ? 1500 km

24
Wave Heating
  • Change in shock flux with height is
  • Energy deposited (dissipated into heat) at height
    h is where

25
Wave Heating
  • Energy also injected by Alfvén waves (through
    Joule heating caused by current through a
    resistive medium)
  • Observations show spatial correlation between
    sites of enhanced chromospheric emission and
    magnetic flux tube structures emerging from
    surface magnetic processes cause much of energy
    dissipation

26
Balance Heating and Cooling
  • Energy loss by radiation through H b-f
    recombination in Lyman continuum (? lt 912 Å) and
    collisional excitation of H
  • In chromosphere, H mainly ionized, primary source
    of electrons
  • for H recombination for H collisional
    excitation
  • Similar relations exist for other ions

27
Radiative Loss Function
  • Below T 15000 K, f(T) is a steep function of T
    because of increasing H ionization
  • Above T 15000 K, H mostly ionized so it no
    longer contributes much to cooling
  • He ionization becomes a cooling source for T gt
    20000 K
  • Above T105 K, most abundant species are totally
    ionized ? slow decline in f(T)

28
Radiative Loss Function
29
Energy Balance
  • In lower transition region (hot) Pg 2
    PeElectron densityRadiation loss
    rate(almost independent of T since f(T)T 2.0)
  • Set T(h) by Einput Erad
  • Suppose Einput Fmech(h) / ?

30
(1) Einput constantT(h) increases with h
Increasing height in outer atmosphere
Each line down corresponds to a 12 drop in Pg or
a 26 drop in Pg2
31
(2) Einput declines slowly with hT(h) still
increases with h
32
(3) Einput declines quickly with h T(h) may not
increase with h
No T increase for damping length ? and pressure
scale height H if? lt H/2H is large in
supergiants so heating in outer atmosphere does
not occur.
33
Temperature Relation for Dwarfs
  • Suppose ? gtgt H in lower transition region so that
    Fmech(h) / ? constant

Constant temperature gradient
34
Heating in the Outer Layers
  • Tgt105 K, rad. losses cannot match heating
  • T increases until loss by conductive flux
    downwards takes over ( wind, rad. loss)
  • Conductive flux (from hot to cool regions by
    faster speeds of hotter particles)
  • Find T(h) from (? 10-6 c.g.s.)

35
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