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The estuary inlet is historically dynamic, with ebb-tidal shoals exhibiting broadly cyclic behaviour on a 10 to 30 yr timescale.
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The spectral signature of total organic carbon content (%TOC) since ~ 7.6 ka matches that of solar forcing over 70 500 yr timescales.
It was found that, for a sub-basin with a higher FF value, precipitation variability can be represented more by runoff variability at less than 2-yr timescales; such a sub-basin is apt to have serious floods.
Relationships of carbon uptake period (CUP) with mean annual temperature (MAT) and integrated net ecosystem CO2 exchange (NEE) at annual (yr) and seasonal (CUP) timescales at ten forest sites.
The timescale is 36 yr at the peak.
The timescale is 6.0 yr at the PZC of olivine (pH = 4.1).
The analyzed results revealed that the attenuation effect of runoff in response to precipitation variability was mainly within the timescale of 2 yr in the Pearl River basin.
Indeed, as is widely known, star-formation activity is always accompanied by dust production on a timescale of 106 yr, very probably through dust production in supernova explosion (e.g., Kozasa and Hasegawa, 1987; Kozasa et al., 1991; Nozawa et al., 2003, 2007, 2008, 2010), though the actual mechanism of dust supply has not been fully understood yet.
Because τg ∝ r2, the timescale is more than 1010 yr.
In these scenarios, emissions grow exponentially in time (with a characteristic timescale t p = 25 – 250 yr) starting from a small initial emission value.
In the Kangra Basin (northwest Sub-Himalaya, India), upper Pleistocene to Holocene alluvial fills and fluvial terraces record periodic fluctuations of sediment supply and transport capacity on timescales of 103 to 105 yr.
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