The instability onset timescale is found to be longer and more variable between runs than the instability decay timescale for a given fuel delivery timescale.
The transient timescales are broadly divided into "short" duration transients, which have fuel delivery timescales shorter than the characteristic instability decay or onset timescales, and "long" duration transients, which have fuel delivery timescales longer than the characteristic instability decay or onset timescales.
Another important index quantifiable in our model is the timescale of the onset.
By studying both Figures9 and10, we conclude that the antisymmetric motion caused by flow-induced instability in a magma-filled dike reasonably explains some characteristics of volcanic tremors, such as the oscillation period and the timescale of the onset.
Therefore, the e-folding time is essentially proportional to the inverse of K 0 ∗, thereby implying that the timescale of the onset of instability is largely controlled by the driving force of the magma flow.
Channel response timescales imply that the onset of relative base level change predates ~3.5 Ma and may have begun as early as ~15 Ma.
Here, we refer to variability that occurs two hours after the onset of undirected singing – a more protracted timescale than the minute-to-minute changes driven by social context, e.g. [44], [45].
Changes in the corrosion process over time were observed for both electrodes, including two different stages: the onset of pit formation followed by a large timescale process in terms of active-passive behavior of the substrates.
In these models, the onset of a seizure results from a dynamical bifurcation of the short timescale dynamics.
Obtaining de novo imprinted expression of a gene that was biallelically expressed at the onset of an experiment is perhaps too hopeful, although at least over the timescale of such an experiment.
