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Small mammal teeth integrate isotopic data over much shorter temporal and spatial scales than large mammal teeth, providing a sensitive measure of local vegetation and placing constraints on the landscape distribution of C3 and C4 plants.
Constraining the parameters on concentrations of groundwater-age tracers (here: tritium) and transient hydraulic-head observations cannot reasonably be done by the EnKF because the concentrations depend on the recharge history over longer times while the head observations have much shorter temporal support.
Diffusion of the components is a fundamental process accompanying whole-organelle dynamics on a much shorter temporal scale.
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Ecological drift, however, generated too much short-term temporal variation in abundance of rare species compared to natural patterns, at time scales between 3 months and two years.
Since rotational correlation times are typically much shorter than the temporal resolution of the system independently of the time bins used, one must acquire ensemble measurements for each sample in order to obtain a good SNR.
Since the rotational correlation times measured in this work are much shorter than the temporal resolution of the system, independently of the time bins that are used, repeating the experiment many times over ensembles of time-averaged trajectories was done in order to construct the time averaged intensity distribution, thus obtaining the best possible SNR.
The time-scale of temporal modulation (approximately 10 ms) was much shorter than the mean inter-spike interval (approximately 1 s).
After the extraction, all temporal segments are concatenated into sequential video with much shorter length than the source sequence.
However, for spaceborne receivers, the typical temporal scales for scintillation-induced signal perturbations are much shorter than in the case of ground-based receivers.
The temporal scales important to a mobile individual's location are likely to be much shorter than a 30 year average [13], [14]; therefore short-term weather may be more appropriate.
Temporal fluctuations in local liquid holdup were seen even in the trickle flow regime; these fluctuations had much shorter time periods than the pore-scale liquid pulses, and are perhaps associated with fluctuations in local surface wetting of the packing elements.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com