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Local Helioseismology

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Title: Local Helioseismology


1
Local Helioseismology
  • LPL/NSO Summer School
  • June 11-15, 2007

2
Global vs Local
  • Global
  • Horizontal interference selects integer values of
    l
  • Entire sun is sampled
  • Spherical harmonics describe waves
  • Cannot get structure as function of longitude
  • Cannot get non-symmetric latitudinal structure
  • One basic technique
  • Valid for l lt 180
  • Local
  • No horizontal interference, can have any
    wavelength
  • Localized volume is sampled
  • Sinusoids or Hankel functions describe waves
  • Longitudinal structure can be determined
  • Non-symmetric latitudinal structure can be
    determined
  • Several techniques
  • Valid for l gt 180

3
History
  • 1987 Sunspots are observed to absorb p-modes
  • 1988 Ring diagram method is invented
  • 1990 Acoustic holography is invented
  • 1993 Time-distance method is invented

4
Sunspot p-mode absorption
  • Decompose observed velocity field in polar
    coordinates into Hankel functions

Hm (1,2) (kr) Jm(kr) i Ym(kr)
5
Sunspot p-mode absorption
  • The quantities Am(k,?) and Bm(k,?) are complex
    numbers containing the power and phase of the
    ingoing (A) and outgoing waves (B).
  • Here m is the polar azimuthal order.
  • Compute absorption
  • a Pin Pout / Pin

6
Results
7
Underlying physics
  • P-modes are scattered by magnetic field into
    shorter (unobserved) wavelengths or other regimes
  • P-mode energy is absorbed by magnetic field and
    transformed into MHD waves

8
Ring Diagrams
  • Based on local plane-wave representation of
    oscillations (The Flat-Sun society)
  • Approximation good for high degrees (l gt 180)
    and shallow depths
  • Allows analysis of wave properties in small
    regions
  • Allows inference of sub-surface flows as function
    of position and depth

9
3-D power spectrum
10
Rings
11
Effect of a flow
12
An extreme flow observed
No tracking, solar rotation rate of 2000 m/s
With tracking to remove rotation
13
Horizontal flows from rings
14
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15
Deriving divergence curl
16
Deriving vertical velocity
17
Vertical velocity
18
Divergence
19
Kinetic Helicity
20
Vorticity below strong flare producers
AR 10069
AR 10486
21
Helicity before a large flare
22
(No Transcript)
23
Time-distance
  • Sound is emitted from a location, travels down,
    and comes back up at some time later and some
    distance away from the source.
  • The time and distance is influenced by the
    conditions of the plasma that the wave travels
    through.

24
Constructing a T-D plot
  • At a given time T, compute the cross-correlation
    between a point and annuli centered on the point
    with different radii D.
  • Repeat for many values of T, plot
    cross-correlation amplitude as a function of T
    and D.
  • Can be done approximately by taking the power
    spectrum of a filtered oscillation power spectrum.

25
Observed time-distance diagram
Cross-correlation function is well described by a
Gabor wave packet
26
T-D diagnostics
  • Changes in travel time are related to subsurface
    conditions (sound speed, flows)
  • Can be inverted to infer the conditions

27
Sound speed below a spot
28
Meridonal flow from TD
1 s 10 m/s
D30 Mm
D65 Mm
D200 Mm
D130 Mm
29
Acoustic Holography in five easy (?) steps
  • Observe wave field in pupil areas
  • Compute a Greens function describing how a
    single impulse at (r,z,t) forms an expanding ring
    at the surface (r',0,t').
  • Convolve Greens function with the observed wave
    field (egression, H blue)
  • Convolve time-reversed Greens function with
    observed wave field (ingression, H- red)
  • Build maps of H and H- over all r, z, t.

30
Greens functions
31
Holography can view the farside of the Sun
AR10808
32
Farside maps
33
Farside Calibration
34
Farside puzzle
  • The same noise structure appears in both MDI
    GONG data, and in both holography TD farside
    analyses.
  • Thus, must be solar in origin.
  • What are they?
  • Magnetic field concentrations that do not reach
    the surface?
  • Large velocity structures?

35
Comparison of methods
  • Rings easy low spatial resolution and shallow
    depth range
  • TD harder higher spatial resolution and greater
    depth range
  • Holography hardest
  • All methods have a trade-off between depth range
    and spatial resolution

36
For more information
  • http//www.hao.ucar.edu/summerschool/program.html
  • Has links to very detailed lecture notes on
    helioseismology and solar internal dynamics
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