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A new transport time scale, recovery time, and a methodology to estimate it by means of numerical models is hereby developed.
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Transport time scales constitute a useful tool for representing the water exchange and transport processes.
These states are found by time-integrating the dynamical equations until the steady-state is reached, and are therefore stationary or statistically steady on both magnetohydrodynamic and transport time-scales.
Recognizing the importance of different varying time scales in the fluvial processes of sediment transport, we introduce the Hilbert–Huang Transform method (HHT) to the field of sediment transport for the time scale analysis.
Long-term changes in depth to water table (30 days before the event) are likely to impact on DOC production, whereas discharge becomes the main control over DOC transport at the time scale of the rainfall/runoff event.
Even companies that are willing to pay substantially more for a higher quality liner shipping service are basically faced by a mode choice and then between modes at either end of the transport time and price scales, rather than a choice between shipping lines or forwarders.
This also alters the frequency dependence of the thermal transport and the characteristic time scale associated with it.
In both the doping or undoping half-cycles, the ion and solvent fluxes normalise with potential scan rate, indicating that they are not subject to kinetic or transport limitations on the moderate time scale of the experiment.
To the extent that the bulk of a Golgi stack is static on the time scale of anterograde transport, this reduces the quantitative demand on retrograde transport of Golgi resident proteins and the need for cisternal maturation.
We show that an increasing magnitude of random surface variability does not appear to have any significant effect on sediment transport over millennial time scales.
This slow detachment could be important in deep subsurface environments where transport on geologic time scales is important, and in some shallow aquifer recharge situations where soils are used to eliminate pathogenic bacteria from sewage effluent.
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