formation of helium lines in prominences
DESCRIPTION
Presentation given to the Solar Physics group at Purple Mountain Observatory, Nanjing.TRANSCRIPT
Formation of Helium lines in solar prominences
Nicolas LabrosseUniversity of Glasgow, Scotland, UK
22 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Outline
•Introduction on solar prominences
•Radiative transfer modelling
–Description of the models
–Influence of the prominence-to-corona transition region (PCTR) on line profiles and intensities
–Influence of the radial motions of the plasma on line profiles and intensities
•Conclusions
32 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
SOHO/EIT
coronaT≥1-2 MKn~108 cm-3
prominencebody
T~8000 Kn~1010 cm-3
Solar prominences
42 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
•How do prominences form?
–What is the magnetic configuration of filament channels, and how is this highly sheared structure created?
–Where does their dense material originate, and how is it maintained?
–How do prominences reach and maintain energy balance with the ambient corona?
–How are the magnetic structure and the plasma dynamics linked?
Puzzles
Labrosse et al. (2010), Mackay et al. (2010)
52 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
•Prominence fine structure and diagnostics
–What are their detailed thermal and magnetic structures?
–How can we use existing (SOHO, Hinode, STEREO, SDO) and future (Solar Orbiter) space missions to obtain the best information on solar prominences?
–Can we construct a prominence model that reproduces the observed emission in optically thin and optically thick lines?
Puzzles
Labrosse et al. (2010), Mackay et al. (2010)
62 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
•Prominence disappearance
–What can observations of heating and activation in prominences tell us about their disappearance?
–Why do filament channels generate the most energetic solar eruptions?
–What tools can we develop to forecast prominence eruptions in a reliable way?
Puzzles
Labrosse et al. (2010), Mackay et al. (2010)
72 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Patsourakos & Vial (2002), Labrosse et al. (2010).
Physical parameters
82 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Temperature, density, ionisation, filling factor, ...Accurate measurements are
crucial to construct realistic models of prominencesdifficult to obtain
prominence plasma not in local thermodynamical equilibrium (non-LTE) because of strong incident radiation coming from the Sun
Large span of measured valuesdepending on the observed structuredepending on the technique used
Non-LTE radiative transfer modelling of prominences sheds light on line formation mechanismshelps to interpret spectroscopic observations / imaging
Plasma parameters
92 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
•Line formation–observations are difficult to understand•Necessity to solve equations–Statistical equilibrium–Radiative transfer including optically thick lines and continua•Non linear and non local coupling between matter and radiation
Non-LTE radiative transfer
102 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Lyman lines of hydrogen form in different parts of the prominence (Heinzel 2007)Optically thick core reveals fine structure close to prominence boundariesOptically thin wings result from integration of several elements along LOSSame for He I and He II resonance linesHe I 584 Å, He I 537 Å, He II 304 Å, He II 256 ÅPlasma out of local thermodynamic equilibrium (LTE)Plasma diagnostics is complexNon-LTE radiative transfer calculations with velocity fields are needed to build realistic prominence models
H and He EUV resonance lines
The prominence model
•1D plane-parallel vertical slabFree parametersGas pressureTemperatureColumn massHeight above the limbRadial velocity
Equations to solvePressure equilibrium, ionisation and statistical equilibria (SE), radiative transfer (RT) for H (20 levels)SE, RT for other elements: He I (29 levels) + He II (4 levels)
Anzer & Heinzel (1999)
The prominence model
122 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Temperature inside the prominence slab for γ=2 (extended PCTR), γ=10, and γ=20 (narrow PCTR). The column mass is M = 5×10−6 g cm−2 and the central temperature is 9000 K.
Prominence-corona transition region (PCTR)
He I: 29 energy levelsHe II: 4 energy levels
76 bound-bound transitions and 33 bound-free transitions561 transitions overall
We can now calculate the emergent radiation.
He I model atom
142 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
He I triplet line intensity ratio depends on prominence altitude
Labrosse & Gouttebroze (2004)
E(10830)/E(D3) vs height above the limb
Intensities and physical parameters
152 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Labrosse et al (2002)
model without transition region
models with transition region
Influence of PCTR on line profiles
H Lyman α He I 584 Å
162 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
T<6000 KT<6000 K
T>16000 KT>16000 K
E(10830)/E(D3) vs optical depth at 504 Å
Labrosse & Gouttebroze (2004)
•PCTR affects formation mechanisms of lines formed in cool parts of the prominence–statistical equilibrium of He I atomic states
Influence of PCTR on He I triplet lines
172 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
MEDOC campaign #13, 15–16/6/2004Observed profiles compared
with grid of 4720 computed models (T, n, ...)
⇩
Ly-β, Ly-ε, and He I 584 Å observed by
SUMER/SOHO
Prominence diagnostic with SUMERBBSO Hα
182 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
ne = 6 108 cm-3 (surface)
ne = 5 109 cm-3 (center)
● Prominence model: 1D plane-parallel slabTemperature profile inside prominence slab(Anzer & Heinzel 1999)
Labrosse, Vial, & Gouttebroze (2006)
Prominence diagnostic with SUMER
192 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Prominence diagnostic with EIS
n(He III)/n(He)
Surface: 0.8Centre: 0
n(HeII)/n(He)
Surface: 0.20Centre: 3.3x10-5
Max = 0.99
np/nH
Surface: 1Centre: 0.94
TemperatureSurface: 105 KCentre: 104 K
See also Heinzel et al. (2008), Labrosse et al. (2011)
202 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
2D models
H ionisation only
H + He ionisation
Gouttebroze & Labrosse (2009)
Ionisation degree in cylindrical prominence
212 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
2D models
6000 K
10000 K
15000 K20000 K30000-50000 K
8000 K
Gouttebroze & Labrosse (2009)
Variation of the ionisation ratio with T
222 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
● Imaging measurements– apparent motion of structure in plane-of-sky
● Doppler shifts in prominence spectra– velocity along line-of-sight
● Doppler dimming / brightening– varies with radial velocity
The full velocity vector may be inferred, but requires at least the radial velocity.
He I model atomHe I model atomDiagnostic of velocity fields
232 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Effects of radial motions•For a simple 2-level atom with photo-excitation–Doppler dimming if the incident line is in emission–Doppler brightening if the incident line is in absorption•If coupling between several atomic levels–situation gets more complex: dimming and brightening–e.g. coupling between first two excited levels of H•Factors determining effects of radial motions–line formation mechanism–details of incident radiation (strength, emission/absorption)
See Heinzel & Rompolt (1987), Gontikakis et al (1997), Labrosse et al (2007, 2008)
Effects of radial motions
V=0 km s-1
V=80 km s-1
V=200 km s-1
V=400 km s-1
He I 584 He II 304 He I 10830
T = 8000 K
T = 15000 K
Labrosse et al. (2007)
252 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
● He II 304 Å line sensitive to Doppler dimming due to radial motion of prominence plasma
Labrosse et al. (2007)
Plasma motions in prominences
262 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Effects on Lyman αDoppler dimming ifLarge temperature
gradient in PCTRNot too denseCool plasma
Doppler dimming of Lyman α line less pronounced when PCTR is extended.increased contribution in line formation of collisional processes in
higher temperature region relative to narrow PCTR case
Results
272 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Effects on Lyman αDoppler dimming ifLarge temperature
gradient in PCTRNot too denseCool plasma
Increasing column mass with all other parameters kept constant means more hot materialcollisional component of Ly-α becomes more important ⇒ the line is
less sensitive to Doppler dimming
Results
282 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Effects on Lyman αDoppler dimming ifLarge temperature
gradient in PCTRNot too denseCool plasma
Increasing temperature of main prominence body increases amount of hot materialcollisional component of Ly-α becomes more important ⇒ the line is
less sensitive to Doppler dimming
Results
292 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Results (5)
Effects on Heliumresonance lines(Same trend as Lyman lines)Doppler dimmingCool plasmaNot too denseLarge temperature
gradient in PCTR
Effects on Helium subordinate lines10830, D3, ... are less sensitive to Doppler dimming/brightening due to weak incident radiation
Results
302 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
(erg
s1 c
m-2 s
r-1 Å
-1)
(PCTR = prominence-to-corona transition region)
E(He I 584) vs. radial velocity
312 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
(erg
s1 c
m-2 s
r-1 Å
-1)
(PCTR = prominence-to-corona transition region)
E(He II 304) vs. radial velocity
322 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
2011-06-10
2010-09-08
Labrosse & McGlinchey (subm)
332 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Comparison with observations
Labrosse & McGlinchey (subm)
342 November 2011 Presentation to Solar Physics Group at Purple Mountain Observatory
Importance of taking into account PCTR–Affects plasma diagnostics from most lines in most cases
Calculations provide constraints for determination of–Opacities–Ionisation degree
– Variations in ionisation degree along LOS can be important
–Radiative losses for energy balance calculations
Compare 2D calculations with observations–Models must be constrained by using several lines (H+He)
Conclusions / Future plans