Using 1D analytical solutions to the groundwater flow equations gives a powerful advantage over the use of more complex models in enabling the sensitivity of the key parameters controlling patterns and timescales of climate groundwater interactions to be analysed analytically.
Each node participates strongly in a few timescales and weakly in the others, but the shape and timescales of the activity patterns emerge from the network topology as a whole and information can flow from one node to another.
The talks will initially focus on the framework and timescale of proper negotiations.
In addition, the influence of taxonomic resolution, from species level data to class level, on spatial patterns was investigated to assess the potential evolutionary timescales of the pattern and for developing cost effective regionally applicable surrogates for biodiversity monitoring.
In total, 113 individuals from 19 localities were sampled, and variations in the chalcone synthase gene (Chs) intron and leafy (Lfy) intron-2 sequences of nuclear DNA were examined in order to assess phylogeographic patterns, the timescales of demographic and evolutionary events, and recent anthropogenic effects.
Spatial and temporal patterns of incision, and the long timescale of steady incision rule out models where geomorphic controls such as climate oscillations, bedrock strength, sediment load effects, or isostatic response to differential denudation are the first order drivers of canyon incision.
These approaches can thus be very sensitive to past demographic events that shape the patterns of ancestral diversity over a timescale of neutral coalescence, which can include quite ancient demographic events.
As evolutionary rate estimates are dependent on their measurement timescales, their values must be used and interpreted under the context of the timescale of rate estimation.
Our numerical simulations reveal the formation of a superimposed traveling wave of hypoxic cells that qualitatively reproduces the experimentally observed patterns and provide an estimate of palisade timescale formation, lifetime, and persistence among other prognostic metrics.
The shorter time describes the timescale of entering the "higher" class, and the longer time describes the timescale of protein deactivation.
