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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 onset timescale is also longer in duration and more variable than the decay timescale at a given fuel delivery timescale, implying that the instability rise process is overall more variable and slower than the instability decay process.
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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.
Less certain is the timescale, with onset of rapid (> 1 mm per year of sea-level rise) collapse for the different simulations within the range of two to nine centuries.
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.
This is consistent with the timescale of disease onset in the mouse model [ 42, 43].
Data in Figures 3 and 4 are displayed with a timescale indicating the verb onset (i.e. the point at which the sentence material was spliced).
Touch was the dominant sensorimotor feature, with >70% spikes occurring in millisecond timescale epochs after touch onset.
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.
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