Difference between revisions of "User:Tohline/Appendix/Ramblings/PPTori"

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==Blaes85==
==Blaes85==


===His Notation===
[http://adsabs.harvard.edu/abs/1985MNRAS.216..553B Blaes (1985)] adopts a [[User:Tohline/SR#Barotropic_Structure|polytropic equation of state]],
<div align="center">
<math>~\frac{\rho}{\rho_c} = \Theta_H^n \, ,</math>
</div>
which gives rise to (slim tori) equilibrium structures for which (see his equation 1.3),
<div align="center">
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>~\Theta_H</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~1 - \frac{1}{\beta^2}\biggl[x^2 + x^3(3\cos\theta - \cos^3\theta) + \mathcal{O}(x^4)  \biggr] \, .</math>
  </td>
</tr>
</table>
</div>
He then adopts a related parameter that is constant on isobaric surfaces, namely,
<div align="center">
<math>\eta^2 \equiv 1 - \Theta_H \, ,</math>
</div>
which is unity at the surface of the torus and which goes to zero at the cross-sectional center of the torus.
===Analytically Prescribed Eigenvector===
From my initial focused reading of the analysis presented by [http://adsabs.harvard.edu/abs/1985MNRAS.216..553B Blaes (1985)], I conclude that, in the infinitely slender torus case, unstable modes in PP tori exhibit eigenvectors of the form,
From my initial focused reading of the analysis presented by [http://adsabs.harvard.edu/abs/1985MNRAS.216..553B Blaes (1985)], I conclude that, in the infinitely slender torus case, unstable modes in PP tori exhibit eigenvectors of the form,
<div align="center">
<div align="center">
Line 41: Line 71:
   </td>
   </td>
   <td align="left">
   <td align="left">
<math>~\biggl\{ f_m(\varpi)e^{-im[\phi_m(\varpi)]} \biggr\}  \, ,</math>
<math>~\biggl\{ f_m(\varpi,\theta)e^{-i[m\phi_m(\varpi) + k\theta]} \biggr\}  \, ,</math>
   </td>
   </td>
</tr>
</tr>
Line 47: Line 77:
</div>
</div>


where we written the perturbation amplitude in a manner that conforms with our [[User:Tohline/Appendix/Ramblings/Azimuthal_Distortions#Figure1|related, but more general discussion]].
where we have written the perturbation amplitude in a manner that conforms with the notation that we have used in  [[User:Tohline/Appendix/Ramblings/Azimuthal_Distortions#Figure1|Figure 1 of a related, but more general discussion]]. As is summarized in &sect;1.3 of Blaes (1985), for "thick" (but, actually, still quite thin) tori, "exactly one exponentially growing mode exists for each value of the azimuthal wavenumber <math>~m</math>," and its complex amplitude takes the following form (see his equation 1.10):
 
<div align="center">
<table border="0" cellpadding="5" align="center">
 
<tr>
  <td align="right">
<math>~f_m(\varpi,\theta)</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
~\beta^2 m^2 \biggl[ 2\eta^2 \cos^2\theta - \frac{3\eta^2}{4(n+1)} - \frac{(4n+1)}{4(n+1)^2}
\pm 4i\biggl(\frac{3}{2n+2}\biggr)^{1/2} \eta\cos\theta\biggr]
+ \mathcal{O}(\beta^3)
</math>
  </td>
</tr>
</table>
</div>


=See Also=
=See Also=

Revision as of 22:35, 18 February 2016

Stability Analyses of PP Tori

Whitworth's (1981) Isothermal Free-Energy Surface
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As has been summarized in an accompanying chapter — also see our related detailed notes — we have been trying to understand why unstable nonaxisymmetric eigenvectors have the shapes that they do in rotating toroidal configurations. For any azimuthal mode, <math>~m</math>, we are referring both to the radial dependence of the distortion amplitude, <math>~f_m(\varpi)</math>, and the radial dependence of the phase function, <math>~\phi_m(\varpi)</math> — the latter is what the Imamura and Hadley collaboration refer to as a "constant phase locus." Some old videos showing the development over time of various self-gravitating "constant phase loci" can be found here; these videos supplement the published work of Woodward, Tohline & Hachisu (1994).

Here, we focus specifically on instabilities that arise in so-called (non-self-gravitating) Papaloizou-Pringle tori and will draw heavily from two publications: (1) Papaloizou & Pringle (1987), MNRAS, 225, 267The dynamical stability of differentially rotating discs.   III. — hereafter, PPIII — and (2) Blaes (1985), MNRAS, 216, 553Oscillations of slender tori.

PP III

Figure 2 extracted without modification from p. 274 of J. C. B. Papaloizou & J. E. Pringle (1987)

"The Dynamical Stability of Differentially Rotating Discs.   III"

MNRAS, vol. 225, pp. 267-283 © The Royal Astronomical Society

Figure 2 from PP III


Blaes85

His Notation

Blaes (1985) adopts a polytropic equation of state,

<math>~\frac{\rho}{\rho_c} = \Theta_H^n \, ,</math>

which gives rise to (slim tori) equilibrium structures for which (see his equation 1.3),

<math>~\Theta_H</math>

<math>~=</math>

<math>~1 - \frac{1}{\beta^2}\biggl[x^2 + x^3(3\cos\theta - \cos^3\theta) + \mathcal{O}(x^4) \biggr] \, .</math>

He then adopts a related parameter that is constant on isobaric surfaces, namely,

<math>\eta^2 \equiv 1 - \Theta_H \, ,</math>

which is unity at the surface of the torus and which goes to zero at the cross-sectional center of the torus.


Analytically Prescribed Eigenvector

From my initial focused reading of the analysis presented by Blaes (1985), I conclude that, in the infinitely slender torus case, unstable modes in PP tori exhibit eigenvectors of the form,

<math>~\biggl[ \frac{W(\eta,\theta)}{C} - 1 \biggr]e^{im\Omega_p t}e^{-y_2 (\Omega_0 t)} </math>

<math>~=</math>

<math>~\biggl\{ f_m(\varpi,\theta)e^{-i[m\phi_m(\varpi) + k\theta]} \biggr\} \, ,</math>

where we have written the perturbation amplitude in a manner that conforms with the notation that we have used in Figure 1 of a related, but more general discussion. As is summarized in §1.3 of Blaes (1985), for "thick" (but, actually, still quite thin) tori, "exactly one exponentially growing mode exists for each value of the azimuthal wavenumber <math>~m</math>," and its complex amplitude takes the following form (see his equation 1.10):

<math>~f_m(\varpi,\theta)</math>

<math>~=</math>

<math> ~\beta^2 m^2 \biggl[ 2\eta^2 \cos^2\theta - \frac{3\eta^2}{4(n+1)} - \frac{(4n+1)}{4(n+1)^2} \pm 4i\biggl(\frac{3}{2n+2}\biggr)^{1/2} \eta\cos\theta\biggr] + \mathcal{O}(\beta^3) </math>

See Also


Whitworth's (1981) Isothermal Free-Energy Surface

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