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Plasma properties
in eruptive prominences
Nicolas Labrosse
University of Glasgow, Scotland, UK
With help from Scott Forrest
Motivation
Understanding how the prominence plasma evolves during an
eruption can shed light on
CME initiation mechanisms
Link between chromosphere and heliosphere
Outline
Effect of plasma motion on emergent radiation
Non-LTE modelling
Results for the He II 304 Å line
Comparison with SDO/AIA observations
Motivation and Outline
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
2
Theoretical calculations have shown that when solar prominences
move away from the surface of the Sun, their radiative output is
affected via the Doppler dimming or brightening effects.
Hyder & Lites (1970), Heinzel & Rompolt (1987), Gontikakis et al (1997), Labrosse et al
(2007, 2008)
Doppler dimming (brightening) is the decrease (increase) in intensity
of a line formed by resonant scattering of the incident radiation from
the Sun due to the radial motion of the plasma.
Mostly strong resonance lines are affected by this effect.
Similar effect used to diagnose solar wind speed
Kohl & Withbroe (1982)
Effects of plasma motions on EPs radiation
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
3
The prominence model
•1D plane-parallel vertical slab
Free parameters
Gas pressure
Temperature
Column mass
Height above the limb
Radial velocity
Equations to solve
Pressure 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)
The prominence model
Multi-level, multi-line
non-LTE modelling
11/06/2013
4
Nicolas Labrosse - IAU Symposium S300, Paris
Doppler dimming/brightening depends on
•Line formation mechanism
•Strength / shape of incident radiation
•Coupling with other energy states
•Coupling with other lines
Effects of plasma motions on EPs radiation
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
5
V=0 km s-1
V=80 km s-1
V=200 km s-1
V=400 km s-1
5
11/06/20
13
T = 8000 K T = 15000 K
Labrosse et al (2010)
6
 He II 304 Å line sensitive to Doppler dimming
 line mostly formed by scattering of incident radiation
coming from the Sun
Plasma motions in prominences
Nicolas Labrosse - IAU Symposium S300, Paris11/06/2013Labrosse et al. (2007)
7
Results (5)
Doppler dimming of He resonance lines stronger if:
Cool plasma
Not too dense
Large temperature
gradient in PCTR
Increasing column mass with all other parameters kept constant
means more hot material → collisional component becomes more
important ⇒ the line is less sensitive to Doppler dimming
Doppler dimming of He resonance lines
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
Constant plasma parameters
Question
Is Doppler dimming observed in eruptive prominences?
11/06/2013
8
Nicolas Labrosse - IAU Symposium S300, Paris
9
2010-06-13
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
SDO/AIA observations
10
2010-06-13
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
SDO/AIA observations
2011-06-10
This study shows that...
Variation of He II 304 intensity with radial velocity
Decreases in some cases, increases in others
Comparison with non-LTE computations
Variation of plasma parameters and Doppler dimming effect
explain changes in He II 304 intensity
11/06/2013
11
Nicolas Labrosse - IAU Symposium S300, Paris
Labrosse & McGlinchey (2012)
Eruption of 19 March 2011 observed by AIA
Plasma diagnostics
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
12
Eruption of 19 March 2011 observed by AIA
Plasma diagnostics
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
13
Surface pressure
decreases during
eruption as EP rises
Perspectives
Extreme Ultraviolet Imager
on Solar Orbiter
•Combining with in-situ data out of the ecliptic
•Better understanding of physical conditions within EPs
•Better understanding of links between EPs and dynamic heliosphere
•EUI will monitor the low atmosphere
counterparts of large-scale solar eruptive
events such as CMEs.
•It will ideally be suited to study
prominence eruptions.
•Using both H Ly-α and He II 304 lines will
add constraints on the models.
11/06/2013
14
Nicolas Labrosse - IAU Symposium S300, Paris
Conclusions
•EP plasma parameters obtained
•minimizing differences between observables and model parameters
•New non-LTE models
•Explain intensity variations by changes in plasma parameters
•Are able to reproduce qualitatively SDO/AIA observations
11/06/2013
15
Nicolas Labrosse - IAU Symposium S300, Paris
TAKK!
Royal Astronomical Society
Specialist Discussion Meeting
Friday 21st February 2014
London
The Life of Solar Prominences
Organisers:
Nicolas Labrosse
Duncan Mackay
Advertisement
11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris
16

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Plasma properties in eruptive prominences

  • 1. Plasma properties in eruptive prominences Nicolas Labrosse University of Glasgow, Scotland, UK With help from Scott Forrest
  • 2. Motivation Understanding how the prominence plasma evolves during an eruption can shed light on CME initiation mechanisms Link between chromosphere and heliosphere Outline Effect of plasma motion on emergent radiation Non-LTE modelling Results for the He II 304 Å line Comparison with SDO/AIA observations Motivation and Outline 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 2
  • 3. Theoretical calculations have shown that when solar prominences move away from the surface of the Sun, their radiative output is affected via the Doppler dimming or brightening effects. Hyder & Lites (1970), Heinzel & Rompolt (1987), Gontikakis et al (1997), Labrosse et al (2007, 2008) Doppler dimming (brightening) is the decrease (increase) in intensity of a line formed by resonant scattering of the incident radiation from the Sun due to the radial motion of the plasma. Mostly strong resonance lines are affected by this effect. Similar effect used to diagnose solar wind speed Kohl & Withbroe (1982) Effects of plasma motions on EPs radiation 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 3
  • 4. The prominence model •1D plane-parallel vertical slab Free parameters Gas pressure Temperature Column mass Height above the limb Radial velocity Equations to solve Pressure 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) The prominence model Multi-level, multi-line non-LTE modelling 11/06/2013 4 Nicolas Labrosse - IAU Symposium S300, Paris
  • 5. Doppler dimming/brightening depends on •Line formation mechanism •Strength / shape of incident radiation •Coupling with other energy states •Coupling with other lines Effects of plasma motions on EPs radiation 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 5 V=0 km s-1 V=80 km s-1 V=200 km s-1 V=400 km s-1 5 11/06/20 13 T = 8000 K T = 15000 K Labrosse et al (2010)
  • 6. 6  He II 304 Å line sensitive to Doppler dimming  line mostly formed by scattering of incident radiation coming from the Sun Plasma motions in prominences Nicolas Labrosse - IAU Symposium S300, Paris11/06/2013Labrosse et al. (2007)
  • 7. 7 Results (5) Doppler dimming of He resonance lines stronger if: Cool plasma Not too dense Large temperature gradient in PCTR Increasing column mass with all other parameters kept constant means more hot material → collisional component becomes more important ⇒ the line is less sensitive to Doppler dimming Doppler dimming of He resonance lines 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris Constant plasma parameters
  • 8. Question Is Doppler dimming observed in eruptive prominences? 11/06/2013 8 Nicolas Labrosse - IAU Symposium S300, Paris
  • 9. 9 2010-06-13 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris SDO/AIA observations
  • 10. 10 2010-06-13 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris SDO/AIA observations 2011-06-10
  • 11. This study shows that... Variation of He II 304 intensity with radial velocity Decreases in some cases, increases in others Comparison with non-LTE computations Variation of plasma parameters and Doppler dimming effect explain changes in He II 304 intensity 11/06/2013 11 Nicolas Labrosse - IAU Symposium S300, Paris Labrosse & McGlinchey (2012)
  • 12. Eruption of 19 March 2011 observed by AIA Plasma diagnostics 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 12
  • 13. Eruption of 19 March 2011 observed by AIA Plasma diagnostics 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 13 Surface pressure decreases during eruption as EP rises
  • 14. Perspectives Extreme Ultraviolet Imager on Solar Orbiter •Combining with in-situ data out of the ecliptic •Better understanding of physical conditions within EPs •Better understanding of links between EPs and dynamic heliosphere •EUI will monitor the low atmosphere counterparts of large-scale solar eruptive events such as CMEs. •It will ideally be suited to study prominence eruptions. •Using both H Ly-α and He II 304 lines will add constraints on the models. 11/06/2013 14 Nicolas Labrosse - IAU Symposium S300, Paris
  • 15. Conclusions •EP plasma parameters obtained •minimizing differences between observables and model parameters •New non-LTE models •Explain intensity variations by changes in plasma parameters •Are able to reproduce qualitatively SDO/AIA observations 11/06/2013 15 Nicolas Labrosse - IAU Symposium S300, Paris TAKK!
  • 16. Royal Astronomical Society Specialist Discussion Meeting Friday 21st February 2014 London The Life of Solar Prominences Organisers: Nicolas Labrosse Duncan Mackay Advertisement 11/06/2013 Nicolas Labrosse - IAU Symposium S300, Paris 16