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Coronal Mass Ejections 4: Modeling CMEs

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Flare energy and the CME kinetic energy must be tightly correlated ... Formed before (Low, 2001) or during (Gosling et al., 1990) eruption? ... – PowerPoint PPT presentation

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Title: Coronal Mass Ejections 4: Modeling CMEs


1
Coronal Mass Ejections 4Modeling CMEs
  • Pre-eruption state
  • (Structure, Evolution, Energy Release)
  • Summary of Models
  • Dynamical Types of CMEs
  • (based in inverse and normal polarity
    configurations)

2
Flare-based CME models
  • Flare represents a pressure pulse.
  • The pulse duration is the duration of the flare
  • Flare has to precede the CMEs
  • Flare energy and the CME kinetic energy must be
    tightly correlated

3
CME Models Prominence Eruption
  • Filament activity precedes eruption (Martin and
    Ramsey, 1972) Recall Sept 11, 2000 event
  • Formation and Eruption of Prominences is central
    to CME models
  • As CME drivers (Filippov, 1996)
  • Reduction of Prominence mass for the onset of
    CMEs (Low and Zhang, 2002)
  • However, Hundhausen (1999) thinks that
    prominences eruptions are not energetically
    favorable to drive CMEs.

4
Aspects of Pre-eruption Phase
  • Structure (Helmet Streamers, Sigmoids, Flux
    Ropes)
  • Evolution (Flux Emergence, Flux cancellation,
    Shear, Twist)
  • Energy Release (Small-scale Heating
    Acceleration Thermal and nonthermal signatures)

5
Three-part structure before eruption (Yohkoh/SXT)
  • Frontal (but sheared)
  • Cavity hidden?
  • Filament core

6
Pre-Eruption StructureSigmoids
  • S- and reverse S-shaped structures in X-ray
    images of Active Regions (Rust Kumar 1996).
  • Erupt more often than non-sigmoidal regions
    (Canfield et al. 1999) Beware of apparent
    sigmoids (Glover et al., 2000)
  • Relation to white light CMEs being studied
  • Coronal counterpart of photospheric shear
    (Ambastha et al., 1993)

7
Sigmoid
  • Yohkoh SXT images of an active region before and
    after CME eruption

8
Pre-eruption Structure Flux ropes
  • Naturally support prominences (Linker et al.,
    2001)
  • Often observed as dark cavity in eclipse pictures
  • Formed before (Low, 2001) or during (Gosling et
    al., 1990) eruption?
  • Interplanetary Magnetic Clouds (MC) are flux
    ropes (Burlaga et al.,1981)
  • MC formed out of filament or cavity of the white
    light CME? (Bothmer Schwenn, 1994 Gopalswamy
    et al., 1998)

9
Cavity in Eclipse Pictures
10
A Cartoon Model of an MC
  • Width, curvature found from multi-spacecraft
    (Helios 1, Voyager 2 Helios 2) Observations
  • Flux Rope Structure from Force Free equilibrium
    calculations
  • (Based on Burlaga,
  • et al 1981)

Ecliptic plane
IMP8, He 2
AXIS
.3 AU
He 1
Mag. Pressure gt Ambient Pressure
Vo2
Width 0.25 AU
11
CMEs and ICMEsA tentative correspondence
  • CMEs Near Sun
  • Shock ?
  • Frontal ?
  • Cavity ?
  • Prominence Core ?
  • Arcade Formation
  • ICMEs near Earth
  • Shock
  • Sheath
  • Ejecta/MC
  • Pressure Plug
  • --------------

12
Pre-eruption Evolution
  • Flux emergence, submergence/cancellation
  • Shear
  • Mass loading (Wolfson, 1989)
  • High coronal reconnection (Antiochos et al.,
    1994 Low and Zhang, 2002)
  • Poloidal flux injection (Chen, 1997 Wu et al.,
    1999)

13
Pre-eruption EvolutionFlux Emergence
  • Substantial Flux emergence near filament before
    eruption polarity of new flux favorable for
    reconnection (Feynman Martin, 1995)
  • - Consistent with numerical simulation studies
    (Chen Shibata, 2000)
  • Significant changes in photospheric flux in
    small areas in the eruption region (Lara et al.,
    2000)
  • CMEs without flux emergence also observed
    (Subramanian Dere, 2001 Wang Sheeley, 1999)
  • Reconnection-favoring flux emergence

14
Weak Dimming Before Eruption
AR-Active Region D-Dimming G- GOES X-ray Flux
15
A transequatorial Eruption
  • EIT 195 A difference image showing dimming at
    0836 UT
  • LASCO image at 0856 UT

16
Pre-eruption Evolution Prolonged Dimming
  • Weak, prolonged dimming for 1 hr (Gopalswamy et
    al., 1999)
  • Small-scale opening of field lines resulting in
    the eruption of underlying structure? (Antiochos
    et al., 1994 Low and Zhang, 2002)

17
Streamer Distension Eruption
18
Pre-eruption Energy Release
19
Pre-eruption Energy Release
  • Signatures of pre-eruption energy release
  • Small-scale heating near filaments, consistent
    with reconnection scenario (Feynman and Martin,
    1995)
  • - Radio bursts near filaments nonthermal energy
    release due to reconnection (Jackson et al.,
    1978 Marque, 2001- Nancay Observations)

20
Energy Release Near Filament
21
Filament Eruption Onset
22
Reconnection-favoring Flux Emergence
23
Simulation supports preeruption Reconnection
(Chen Shibata 2000)
  • Top Flux emergence under the filament
  • Bottom flux emergence from the side

24
Summary of Numerical Models of CMEs
Caution This table is incomplete, mainly
initiation
25
Flux-rope expulsion Inverse Configuration
Flux-rope field Surface field in the opposite
direction
Low and Zhang, 2002
Jf ltgtJcs RC not needed
26
Example from SXR H-alpha
Pre-eruption
Post-eruption
27
Flux-rope expulsion Normal Configuration
Flux-rope field Surface field in the Same
direction
Low and Zhang, 2002
Jf gtltJcs RC needed
28
CMEs from Normal Inv Ropes
  • Normal Polarity
  • CS above flux rope
  • Rapid acceleration
  • No arcade?
  • Deceleration possible from eruptive config
  • FR-ambient reconnection
  • Inverse Polarity
  • CS below flux rope
  • Gradual acceleration
  • Post-ruption arcades
  • No deceleration expected
  • No FR-ambient field reconnection

29
Summary of Forces
  • Propelling Forces Hoop force, hydromagnetic
    buoyancy force. Problem How these are
    distributed in the pre-eruption stage and how the
    balance is lost.
  • Retarding forces Gravity (M), Coronal Drag (V)

30
Fe Ratio Can Identify CME
  • Fe Ratio - the fraction of high-charge state (
    16) Fe ion density relative to the total Fe
    density in all charge states (plotted ratio X
    200) (Lepri et al., 2001)
  • Short-lived intense geomagnetic storm follows
    immediately after the shock ? sheath

31
Prominences
  • Type A,B,C filament
  • A bipolar, B-between bipolar, C-between polar
    crown and active belt B most common (2/3 F.
    Tang)
  • Polarity Normal (KS), Inverse (KR)
  • Chirality (Foukal, Marin)
  • Sinister/southern dextral/northern does not
    tell you about helicity
  • Sinistral normal ? RH
  • F Channel Chae et al. (2001)

32
Prom B
  • Zirin Severny (1961) first meas
  • On disk Harvey (2001)
  • Hanle depolarization by local B Leroy et al.
    (1977) On disk Lin (1998)

33
Eruption
  • Flux Cancellation bifurcation of F
  • What causes formation? Are they flux rope?
    Tightly bound flux
  • What activates filament?
  • Can the statistics of Leroy taken for granted
  • Is the global pattern fundamental for Phys?

34
Flares
  • Posflare loops
  • Bastille day event two eruptions?
  • Standard flare model Sturrock (1968) single
    bipolar region
  • Cusp in Yohkoh RC?
  • Yokoyamas reconnection example
  • Loop intercation model different from standard
    flare model?

35
Negative Associations
  • Continuous vs explosive
  • Two step RC 1. Cancellation 2. Explosive flare
    is second, Mathew Ambastha (2000), Ji et al
    (2001a,b,c), Livinenko (1999) H.Wang et al.
    (2002)
  • Q What is the preflare config?
  • Irreversible Impulsive changes?
  • Primary release site?
  • Zhou et al., 2002 92 PE ass. With CMEs
  • 990205 flux rope

36
Flux Rope
  • Curren carrying emerging flux (Chen, 2001)
  • Filament (Rsut Kumar, 1994) continuos dist. Of
    dip
  • Cavity (Low, 1996) van Ball Martens (1989)
  • Plasmoid (Shibata, 2001)
  • Yan et al. (2001)
  • Nature of dimming
  • Large-scale field structure hosting CMEs TIL,
    Long channel, Sigmoid
  • Cancellation only detectable magnetic change
  • Forbes et al.
  • 10filament eruption
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