wiki:ShockedClumps

Version 22 (modified by Jonathan, 14 years ago) ( diff )

Shocked Clumps

Common params

namb 250 cc-1
Tamb 100 K
Rclump 100 AU

Run Params

Run vwind (km/s) tcc (yr) final time (yr) Tbow (K) Ttrans (K) Lbow (Rc) Ltrans (Rc)
A 50 10 3.00 yr 568.9 yr 5.64e+04 5.64e+03 2.73e-01 7.86e+00
B 100 10 1.50 yr 248.4 yr 2.26e+04 2.26e+03 8.10e-01 1.16e-01
C 200 10 .750 yr 142.2 yr 9.02e+05 9.02e+04 3.93e+01 3.34e-02
D 400 10 .375 yr 71.1 yr 3.61e+06 3.61e+05 1.88e+03 2.11e-01
E 800 10 .1875 yr 35.5 yr 1.44e+07 1.44e+06 1.40e+04 2.30e+01
F 200 100 .750 yr 142.2 yr 9.02e+05 9.02e+04 3.93e+01 1.41e+00
G 200 10 .750 yr 142.2 yr 9.02e+05 9.02e+04 inf inf

Shock Structure

Bow Shock

For the bow shock temperature, we assume that this shock is stationary with respect to the flow in which case the material flowing into the shock will see a shock travelling at so

Wind Shock

However, before the wind reaches the clump it first shocks against the stationary ambient and produces a wind shock. To solve for the speed and temperature of this wind shock we first switch to a reference frame in which both the wind and the ambient are colliding at

If we shift to this reference frame, we then know from symmetry that the postshock velocity must be 0. Using this along with the pre-shock conditions we can solve for the post-shock density, pressure, and the shock speed by Applying the Rankine-Hugoniot jump conditions at the interface

Or we can assume that the shock is adiabatic with a high mach number which then gives us that in which case or in this case or in the ambient frame of reference . The backward facing shock would then have velocity so the forward shock would be travelling at twice the speed as the backward shock and the shocked region would be as large as the unshocked inflow region - which is visible in the non-cooling bow runs. In any event the velocity of the wind shock is then … On a side note, if you run material into a wall at a high supersonic velocity , the shocked temperature ends up being .

Eventually this wind shock slams into the shock and should produce a reflected shock. Using the same analysis we get that the reflected shock temperature within the windshock should be however we have ignored the fact that this windshock material is already shocked, so this reflected shock would be fairly weak and some of the assumptions used above break down. Eventually this reflected shock breaks out of the windshock and into the ambient where it now sees cold material flowing in at and forms the bow shock.

Transmitted Shock

And finally we have

Cloud crushing time

In the strongly cooling case, the forward and reverse wind shock collapse to the center of the shock which is travelling at . It makes sense to use this as the wind speed of the 'shock' for calculating the cloud crushing time etc… Under these assumptions, the shock is first incident on the clump at . Furthermore the cloud crushing time is

Temperature lineout for non-cooling case

Below is a snapshot from this movie that shows the evolution of the shock structure along the axis. Also plotted are the temperatures for the bow, wind, and transmitted shocks calculated above. Temperature lineout of 800_10 run before wrap around shock hits axis.

Cooling Lengths

ZonePlot of DMCooling for runs

A naive calculation of Lshock using the instantaneous cooling rate at Tshock would implies that run A is bow only, run B is both, runs C & D are trans only, run E is neither, and that run F is marginally transonly only. However it does appear that run F has both a cooling bow shock and transmitted shock. To understand the discrepancy we should consider the following figure where we have plotted the cooling lengths in units of clump radius as a function of wind velocity for the bow shock as well as for the transmitted shocks with = 10 & 100

Not here we have calculated the cooling length by integrating along the cooling curve until the temperature has dropped by half. To see the same curve but using the instantaneous cooling rate see this image

Cooling lengths of bow shock, & transmitted shock for chi=10, 100 in units of clump radius generated by interpolating the cooling curve...

If we consider where the blue curve intersects with a wind speed of 200 km/s, we see that the slope of the cooling length as a function of velocity (or temperature) is very high. As the bow shock cools it effectively slides to the left and the cooling length becomes around .1 Rc. This explains the dramatic behavior of the ambient shock in run F. The transmitted shock also follows a similar behavior transitioning from marginally cooling to a cooling length of approx .1 Rc as well.

Run E which is also very curious because while neither the bow shock nor the transmitted shock initially is cooling, the intersection of the transmitted shock with the wrap around shock triggers dramatic cooling and fragmentation. From the intersection of the red line with 800 km/s we see that the transmitted shock is on the same region of the cooling curve as the bow shock was for run F and once it begins to cool the cooling length drops from 10 Rc to .01 Rc.

Images and Movies

A 50 10 (bow only) D 400 10 (clump only) E 800 10 (neither ) F 200 100 (both)
movie movie zoom movie movie zoom
5 50_10_5400_10_5800_10_5200_100_5
10 50_10_10400_10_10800_10_10200_100_10
15 50_10_15400_10_15800_10_15200_100_15
20 50_10_20400_10_20800_10_20200_100_20
25 50_10_25400_10_25800_10_25200_100_25
30 50_10_30 400_10_30 800_10_30

Paper Figures

Zone Plots

Analytic Zone Plot

Analytic Zone Plot for single parameter regime

Analytic Zone Plot Series

Analytic Zone Plot for 4 different parameter regimes

Raymond Zone Plot Series with varying clump size

Series of zone plots with different clump radii generated with data from Raymond 1D sims

Schlieriens

We know have data from a run at 200 km/s with a density constrast of 10 with and without cooling. I've replaced the 800 km/s run with the 200 km/s without cooling and the run with a density contrast of 100 with one with a density constrast of 10.

Below are schlieriens of runs G, A, C, D at frames 7, 11, and 15 at t = .6957, 1.4546, 2.2136 tcc

Schlierien comparison of winds at 200km/s w/o cooling, 50 km/s, 100 km/s, and 200 km/s

Here are the previous schlieriens

Schlieriens of density at three different frames matching the transmitted shock position

Schlierien plot synchronized by transmitted shock position at chi=10 frames 7 11 and 23

Schlieriens of density at three different frames matching the bow shock position

Schlierien plot synchronized by bow shock position at frames 7 11 and 23

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