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This steady state is unique and stable.
The approach to this steady state was also predicted.
this steady state probability is given by solving the set of balance equations[20].
This steady state coexists with the typical low activity equilibrium and oscillations.
An analytical expression for calculating this steady state velocity was presented as a function of the gait pattern parameters.
If the system relaxes into a steady state, this steady state must be identical to the long-time average (7).
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In recent years, this steady-state conceptual view of the oceans has undergone some modification.
This steady-state model was derived from the dynamic model proposed by Choulak (2004).
To compensate for this steady-state error, we consider two secondary control strategies.
Hence, the successful experimental search for this steady-state pattern in real systems seems doubtful.
Here, we use this steady-state information to identify regions of stable pitch frequency and high harmonicity.
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