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Holbrook, N. J., Goodwin, I. D., McGregor, S., Molina, E. & Power, S. B. ENSO to multi-decadal time scale changes in East Australian Current transports and Fort Denison sea level: oceanic Rossby waves as the connecting mechanism.
When processing the SCPC CAZAC waveform in (3) using the AF in (2), the narrowband assumption is used that states that the transmitted waveform does not experience any time scale changes due to target motion.
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Over longer time scales, changes in precipitation regimes will alter relative abundances, allow new species to colonize, and cause the local extirpation of current members of the community [8].
On evolutionary time scales, changes in the equilibrium of a conformational ensemble may result in highly different conformational ensembles among homologous proteins (Siltberg-Liberles et al. 2011).
Specifically, such time-frequency distortions can be modeled by time scaling (or linear speed change) which modifies both duration (or speed) and pitch of music signals by resampling, time stretching (or time scale modification (TSM)) which changes only the duration using certain algorithms, and pitch shifting which merely causes the change of pitch.
As such a combination of short time-scale mechanisms in combination with adaptive routing to handle larger time-scale changes could be an appropriate fully adaptive solution.
Short time-scale changes must be handled by other mechanisms, but care should be taken that different mechanisms at different time scales and different layers do not become counterproductive.
We observe that varying one of the slow time-scales changes the boundaries of different dynamic behaviors.
Knowing that proprioceptive inputs contribute to short time-scale postural adjustments [43], this decrease in complexity, indicated by the increase in DFA α-values, most likely represents increased predominance of slow time-scale changes in posture that occur when proprioceptive information is reduced.
Also, the algorithm was not as robust against time scale modification (TSM) and speed change [8].
The surface ocean is subject to both dynamic changes on a short time scale and changes caused by global warming and ocean acidification [ 15].
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