Schneibster
Unregistered
- Joined
- Oct 4, 2005
- Messages
- 3,966
2.5% of a small difference is smaller than 2.5% of a big difference.Could be. I'm aware that it's (roughly speaking) an exponential dropoff. Of course what this means is that at any given altitude, there will only be a fixed percentage difference in pressure between that altitude and a fixed distance above that. 187 meters is something like a 2.5% difference--seems small to me.
A bolide is an unusually bright meteor that leaves a trail.Neat. Might I ask specifically what your definition of "bolide" is? I've found several of them on the 'net, including one that only includes impactors.
That's the bottom of the stratosphere, not the top. The top is at 30-50km. That's even a bit low for the bottom; it's at 8-17km. It sounds like you're talking about the tropopause.I thought it was much lower than that--5-10 km, not 30 km or more?
We are in agreement, then.Well, I will happily grant that if the heating occurs within tens of milliseconds, then you indeed should expect some rather energetic EM radiation, including X-rays.
Consider a re-entering spacecraft, which loses contact with the ground because it is surrounded by ionized gas. This is because of the heat of atmospheric friction, and that's in the ionosphere, not even in the stratosphere.I am still not entirely convinced that this would happen for a 30 m object, but this opinion is largely based on my ignorance of hypervelocity objects in the atmosphere. Perhaps sometime I will write a simple simulation that shows the balance between radiation and aerodynamic heating.
- Dr. Trintignant