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Global Helioseismology 2: Results

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Title: Global Helioseismology 2: Results


1
Global Helioseismology 2 Results
  • Rachel Howe, NSO

2
Synopsis
  • Mode parameters, mode physics, and the solar
    cycle
  • Frequency changes
  • Width, amplitude and asymmetry
  • Internal Structure
  • Internal Rotation
  • The overall picture
  • Temporal variations

3
Frequency shifts with solar cycle
4
Frequency shift sensitivity
5
Even splitting coefficients follow magnetic
activity distribution
6
Localized global frequency shifts
7
High-degree frequency shifts
  • Mode frequencies are higher in active regions
  • (Hindman et al, 2000).

8
High-degree Frequency Sensitivity
  • High-frequency modes can have anticorrelation
    with activity level.

9
Note on Frequency Shifts
  • Sensitivity depends mostly on frequency.
  • Shifts are strongly localized to active regions.
  • The effect is heavily dominated by the magnetic
    features at the surface.
  • The exact mechanism (sound-speed? temperature?
    cavity size? magnetic field?) is still under
    debate.

10
Mode Parameters
  • Width is inversely proportional to lifetime
  • Area under peak mode power (amplitude)
  • Power x lifetime Energy Supply Rate

11
Low-degree Mode Width
  • l0, 1, 2 modes from GONG and BiSON

12
Low-degree Mode Amplitude
  • l0, 1, 2 modes from GONG and BiSON

13
Medium-degree mode parameters
  • From Libbrecht, 1988.

14
Mode Energy Varies With Activity
15
High-degree Mode Amplitude
  • Amplitude from ring-diagram analysis is
    suppressed in active regions.

16
High degree mode amplitude
  • But at higher frequencies peak amplitude
    increases with frequency.

17
Sensitivity varies with frequency
18
Mode Width Varies With Activity
19
High-degree mode width
  • Peaks are broader (shorter lifetimes) in active
    regions.

20
High-degree mode width
  • But at higher frequencies, linewidth decreases
    with activity.

21
Sensitivity varies with frequency
22
Reminder
  • Oscillations excited by granulation.
  • Might expect active regions to make a difference.

23
Summary
  • For trapped modes, power and lifetime decrease
    with activity.
  • High frequency non-trapped modes behave
    differently, increasing power and lifetime in
    active regions.
  • The boundary between trapped and untrapped may
    change with activity level.

24
Summary of the Summary
  • Rule 1 Everything varies with everything else.
  • Rule 2 Its more complicated than that.

25
Structure Inversion Results
26
Results of OLA inversion of solar data
Sound speed
Fractional differences between Sun and a model,
in sense (Sun minus model) from BiSON LOWL
data (Basu et al. 1997, MNRAS 291, 243)
Density
27
Constraining solar structure models
  • Neutrino discrepancy solved
  • All exotic models inconsistent with measured
    frequencies
  • Standard model pretty good, but still discrepancy
    below CZ
  • Near surface poorly understood

28
Depth of convection zone
From an inversion for sound speed, can calculate
W, which in the convection zone takes the
approximately constant value -(G1-1) (except in
regions of partial ionization).
inversion
model
Seismically determined location of base of
convection zone is rcz/R 0.713 /- 0.004
29
Helium abundance
From inversions using u and Y, Richard et
al. (1998) determined helium abundance in the
solar convection zone to be 0.248 /- 0.002
Can also (try to) use the HeII bump in W at
r0.98R either by fitting or from its
signature as a sharp feature
W
30
2-d structure inversion from MDI
  • Based on early (1996) MDI data

31
Sound-speed Inversion Results below the surface
32
2-d structure remarks
  • Most solar-cycle variation comes from
    near-surface activity and goes into the surface
    term in inversions.
  • Is something strange (hot) happening around 60
    degrees?

33
Rotation Inversion Results
  • The mean rotation profile
  • Residuals
  • Phase and amplitude from sinusoid fits

34
Rotation Inversion Results
35
Rotation Inversion Results
36
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37
Penetrating flows
  • Vorontsov et al 2002, Science
  • MDI, new inversion technique
  • High-latitude changes go deep
  • Low-latitude flows down to at least 0.92R

38
Zonal Flow Pattern
39
Zonal Flow Pattern
40
Zonal Flow Patterns (Time-Radius)
15
30
0
45
60
MDI OLA
MDI RLS
GONG RLS
41
Sinusoid Fits
  • W(r,q)W0(r,q)A(r,q)sinwtf(r,q)
  • Phase (left) and amplitude (right) for 11yr
    sinusoid fits to zonal flow variation
  • Fit can be improved by including 2nd harmonic.

MDI OLA
MDI RLS
GONG RLS
42
Zonal Flows the Movie
  • Movie based on two-harmonic sinusoid fit to
    rotation residuals.

43
Rotation the Movie
  • Red is faster rotation, green/blue slower.
  • Different colour tables in upper and lower
    convection zone.

44
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45
Flows and Magnetic Activity (Smoothed)
46
Summary of Rotation Results
  • Shear layer (tachocline) divides
    differentially-rotating convection zone from
    solidly-rotating radiative interior.
  • Near-surface shear has fastest rotation around
    0.95R.
  • Differential pattern persists through convection
    zone, not quite radially.
  • Zonal flow pattern, or torsional oscillation
    penetrates much of convection zone.
  • Pattern has (weak) equatorward and (strong)
    poleward branches.
  • Pattern in the interior is phase-shifted, leading
    the surface pattern.

47
Credits
  • Thanks to
  • W. J. Chaplin (Birmingham)
  • J. Christensen-Dalsgaard (Aarhus)
  • B. Hindman (CU Boulder)
  • J. W. Leibacher (NSO Tucson)
  • M. J. Thompson (Sheffield)

48
Further Reading
(Coming June 27)
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