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Supergranulation Waves in the Subsurface Shear Layer Cristina Green Alexander Kosovichev Stanford University

Supergranulation Waves in the Subsurface Shear Layer

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Supergranulation Waves in the Subsurface Shear Layer. Cristina Green Alexander Kosovichev Stanford University. Observations. Supergranulation pattern appears to rotate faster than plasma. Gizon et al. (2003) observed supergranulation waves with periods of 6-9 days and phase speeds ~65 m/s. - PowerPoint PPT Presentation

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Page 1: Supergranulation Waves in the Subsurface Shear Layer

Supergranulation Waves in the Subsurface Shear Layer

Cristina Green

Alexander Kosovichev

Stanford University

Page 2: Supergranulation Waves in the Subsurface Shear Layer

Observations

• Supergranulation pattern appears to rotate faster than plasma.

• Gizon et al. (2003) observed supergranulation waves with periods of 6-9 days and phase speeds ~65 m/s.

Gizon, L., Duvall, T. L. Jr, Schou, J. Wave-like properties of solar supergranulation. Nature 421, 43-44 (2003)

Page 3: Supergranulation Waves in the Subsurface Shear Layer

Dispersion Relation:

Figure from Gizon et al. (2003)

Page 4: Supergranulation Waves in the Subsurface Shear Layer

Motivation

• Want to investigate the effect of subsurface shear flow on convective modes.

• Main result is that convective modes become running waves in the presence of shear.

• Goal to calculate phase speed of convective modes and compare with observations.

Page 5: Supergranulation Waves in the Subsurface Shear Layer

Formulation

• First solve this problem in the linear approximation.

• Problem was first formulated by Adam (1977).

Adam, J. A. Hydrodynamic Instability of Convectively Unstable Atmospheres in Shear Flow. Astrophysics and Space Science 50, 493-514 (1977)

Page 6: Supergranulation Waves in the Subsurface Shear Layer

Physical situation:

Figure from Adam (1977)

Page 7: Supergranulation Waves in the Subsurface Shear Layer

Model

Adam (1977): idealized physical situation

• ignored thermal diffusivity and viscosity

• imposed negative entropy gradient

• convectively unstable region bounded above and below by convectively stable regions

Page 8: Supergranulation Waves in the Subsurface Shear Layer

• Assume that over depth of order of unstable region, regions above and below are stable

• Reasonable for supergranular/granular interaction

• Justified in taking supergranular motion to be represented by shear flow in sub-photospheric granular convection zone

Page 9: Supergranulation Waves in the Subsurface Shear Layer

Equations

• Derived from linearized equations of continuity, motion and adiabatic compressibility.

• Equations in terms of pressure perturbation and vertical displacement.

• Both treated as periodic functions of horizontal coordinates and time.

Page 10: Supergranulation Waves in the Subsurface Shear Layer

Linearized Equations

0010

1 dz

duu

dt

dz

x

p

dz

dUu

dt

duz

x

1010

10

y

p

dt

du y

110

gz

p

dt

du z1

110

dz

du

dt

dc

dz

dpu

dt

dpzz

01

120

01

1

x

Utdt

d0

Page 11: Supergranulation Waves in the Subsurface Shear Layer

020

2002

0

qnkUρ p

c

g

dz

d

01 2

020

2102

0

20

pkUω

ckρ q

c

g

dz

d kUω

Equations

Solve for frequencies at given wavenumbers using finite differences.

Page 12: Supergranulation Waves in the Subsurface Shear Layer

dz

dg

c

gn 0

020

220

Brunt-Väisälä frequency:

Page 13: Supergranulation Waves in the Subsurface Shear Layer

Consider range of k corresponding to typical supergranulation size.

Page 14: Supergranulation Waves in the Subsurface Shear Layer
Page 15: Supergranulation Waves in the Subsurface Shear Layer

Solar Model Shear Flow

Page 16: Supergranulation Waves in the Subsurface Shear Layer
Page 17: Supergranulation Waves in the Subsurface Shear Layer

Calculate phase speeds,

for first three convective modes. Subtract surface speed, to observe how much the phase speed of the convective waves exceeds the plasma speed.

Phase Speeds

ku

2

Page 18: Supergranulation Waves in the Subsurface Shear Layer
Page 19: Supergranulation Waves in the Subsurface Shear Layer

Shear Gradient

• Phase speed dependence on gradient of shear flow profile.

• Calculate with series of shear profiles, all with zero surface speed and constant gradients.

Page 20: Supergranulation Waves in the Subsurface Shear Layer
Page 21: Supergranulation Waves in the Subsurface Shear Layer

Eigenfunctions

Page 22: Supergranulation Waves in the Subsurface Shear Layer

With Shear Flow:

Page 23: Supergranulation Waves in the Subsurface Shear Layer

Conclusions

• Model shows evidence of wave behaviour of supergranulation, with supergranules travelling faster than plasma.

• The wave behaviour is caused by the subsurface shear flow.

• Speeds obtained still slower than observations. Need to consider non-linear model.