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Part 1 - Centrifugal Blackholes (cont) |
ARGUMENT
0506
BROUGHT
FORWARD
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ARGUMENT 0504: Any
acceleration in a teelosphere teel equates to a movement toward the
equator and a deceleration equates to a movement toward the poles.
- ARGUMENT
0505: Teels in a blackhole's teelosphere stratify in altitude and
latitude according to their realspeed relative to each other with
the fastest low over the equator and the slowest high over the
poles.
REASONING:
- Teels
are stratified into streams but collisions still occur which result
in the acceleration of one teel and the deceleration of the other.
- Collisions
over the equator cannot result in the fastest teel moving “toward”
the equator so it must move upward.
- Collisions
over the poles cannot result in the slowest teel moving “toward”
the poles so it must move downward.
- Thus
the path of least resistance for a teelosphere
is a centrifugal flow pattern.
- In
a centrifugal flow pattern, fast teels stream toward the equator at
low level, rise, decelerate, stream back toward the poles at high
level, fall, accelerate, and stream back toward the equator at low
level, and so on.
CONCLUSION:
- The
default flow pattern for a blackhole teelosphere is centrifugal with
low level teels streaming toward the equator and high level teels
streaming toward the poles.
| GLOSSARY:
- centrifugal blackhole: The
teelosphere of a centrifugal blackhole responds to the spin of the
blackhole's teelcore by rising at the equator, moving to the poles at
high level, sinking at the poles, and returning to the equator at low level (see also axial blackhole).
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