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Real human body parts (i.e. organs, cellular components, enzymes) have biological functions which have various timescale to complete the function.
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The North Atlantic has been the location of active research on climate oscillations at various timescales.
After establishing such groupings, in some cases with class membership changing depending on the location of the trajectory in phase space, we used a non-rigorous GSPT approach to elucidate the roles of various timescale-based subsystems and their bifurcation structures in producing sigh-like dynamics.
Such correlations appear at various timescales.
According to the soliton solution, we research the solitary wave profiles for various timescales and the collisions between two waves with different velocities and various timescales.
Sealing and unsealing is common and occurs repeatedly at various timescales in phreatic systems.
In Figure 2, the collisions between two waves with different velocities and various timescales appear.
In this section, we display the soliton solutions and the solitary wave profiles for various timescales in Figure 1.
Figure 2 The collisions between two waves with different velocities for (pmb{c=0.5}) and (pmb{c=5}), respectively, and various timescales for (pmb{t=0.08}), (pmb{t=0.1}), and (pmb{t=0.2}), respectively.
Some systems (e.g., Ruapehu, Poás) can produce both type 1 and type 2 eruptions, and all systems can undergo sealing at various timescales.
Decision makers with different responsibilities require hazard information at various timescales (black bars on Fig. 4A) and levels of detail, with an emphasis on uncertainty.
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