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Useful Links
Project Pages (Stuff currently on my plate - ordered by priority)
- Scrambler Paper
- Gravitationally induced turbulence
- Colliding Flows
- Thermally Unstable clouds
- MHD Clumps
- Mapping Out Cooling Regimes for Shocked Clumps
- The Morphological Impact of Cooling on Turbulence
Recent Blog Entries
Literature survey:
Klessen Heitsch MacLow 2000
- Collapse can only be prevented with unrealistically short wavelength driving
- Realistic driving ength gives observed core formation rates
- Discuss various dispersion relations for jeans analysis with turbulence
- Reference Bonazzola 1992 which has a critical spectra for support of alpha = 3 (outflow turb?)
- SPH and Lagrangian 3D Hydro Periodic 64 Jeans Masses
- Drive with various scales for 1 crossing time and then switch on self-gravity
- Forcing patterns described in MacLow 1998 and 1999
Heitsch Maclow Klessen 2000
- Similar to above but with MHD
- Density contrasts are lessened because of magnetic pressure
- Flow is organized into sheets - more clustered
Ossenkiof Klessen Heitsch
- Applied delta variance technique to self gravitating turbulence
- Periodic Box
- Density spectra has positive slope when self-gravity is important
- Propose to compare it with dust observations instead of 12CO to have a higher density contrast range
- 2563
Heitsch et al 2005
- Non-gravitating hydro colliding flows with cooling
- NTSI, KH, TI, but no discussion of Richtmeyer-Meshkov instability (Impulsive-accelerating RT instability)
- Look at 'core' properties (though 2D and no SG)
Heitsch et al 2006
Random Ruminations
So setting up the initial solution can be accomplished by the following:
First start with the assumption that the retarted time is the current time
DO
Calculate the displacement vector from the primary at the retarded time
Calculate the wind normal so that
It is possible to solve
for the unit vector
Once we have an estimate for
we can improve the estimate by modifying the trajectory to account for the gravity from the secondary as follows:
Calculate the wind velocity from the primary
Now solve for the trajectory from the primary that leaves at
at velocity taking into account the force from the secondary.
Determine the path's distance of closest approach to
and call that
Estimate the change in initial velocity needed
And then solve for the unit vector that gives that direction
Cycle until
Update the retarded time using the new distance and wind speed
END DO
The only problem occurs when there are multiple solutions for the retarded time…
This will occur once we reach distances of order
If we switch to a rotating frame that rotates counter to the orbit so the angular speed is
, then
and
so that
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