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- From: Richard.Mathews@West.Sun.COM (Richard M. Mathews)
- Newsgroups: sci.physics
- Subject: Re: Satellite spying
- Date: 25 Aug 1992 12:45:20 -0700
- Organization: Sunsoft Inc., Los Angeles, CA.
- Lines: 28
- Sender: richard@smaug.West.Sun.COM (Richard Mathews)
- Message-ID: <17e2kgINN5k4@smaug.West.Sun.COM>
- References: <9223715.21857@mulga.cs.mu.OZ.AU> <4720047@hpcc01.corp.hp.com> <17chpmINNma3@agate.berkeley.edu>
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-
- ted@physics3 (Emory F. Bunn) writes:
- >Even taking into
- >account the fact that this is a very rough calculation, that seems
- >hard to believe. It's significantly better than the best ground-based
- >telescopes, which get about 0.5 arc-second resolution on a good day.
- >Naively, one would expect those two resolutions to be comparable,
- >since they're both limited by "seeing" (atmospheric turbulence).
-
- Atmospheric seeing effects instruments looking up more than those looking
- down because most of the air which causes the blurring is closer to the
- former.
-
- Consider a cone of light going from a source to a telescope. The apex
- of the cone is at the source, and the base is the objective of the scope.
- To determine seeing, you need to know how much the wavefront is deformed
- as it reaches the scope. With a telescope which is looking up, the wide
- part of the cone is deep in the atmosphere, and the light travel time
- can be substantially different through the different air masses. On the
- other hand, when looking down, it is the narrow part of the cone which
- is deep in the atmosphere. All the light passes through essentially the
- same air masses, so the travel time is comparatively constant. By the
- time the light diverges far apart at the wide end of the cone, the air
- is too thin to make much difference.
-
- Richard M. Mathews Lietuva laisva = Free Lithuania
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