Field research has established that groundwater upwellings provide stable environments (reduced variability in flow and temperature regimes, and reduced channel slope and bed movement), with high water tables, supporting vegetation growth on otherwise barren glacial floodplains.
The study was designed with emphasis on shade cover variation within each of the two study areas, while minimizing the variability of environment, agronomic management other than shade, and post-harvest processing.
As indicated here, a close examination of EPR line shapes and their variability with environment indicates that the SNARE motif of synaptobrevin is in equilibrium between the aqueous phase and the lipid interface.
Their use on a regional scale is generally constrained, however, by a lack of information on the spatial and temporal variability of environment-related input variables (e.g., soil) and agricultural practices (e.g., sowing dates) that influence crop yields.
Variability among environments within TPE (locations and seasons) is particularly common in rice.
However, an alternative interpretation of these results is possible if we think of high variability across environments not as low robustness, but rather as high, and potentially adaptive, phenotypic plasticity.
Inter-annual variability in environments creates pulsed-resource dynamics that affect many animal populations [ 11- 13] by affecting primary productivity [ 14- 16] and the frequency and intensity of landscape disturbances [ 17, 18].
The variability in physical environment variables may have been higher if participants had originated from different areas.
It is well known that the assumption of almost periodicity of the coefficients in (1.1) is a way of incorporating the time-dependent variability of the environment, especially when the factors of the environment exhibit periodical changes with not necessarily commensurate periods, such as weather, food, mating habits, harvest, etc.
The assumption of almost periodicity is a way of incorporating the time dependent variability of the environment, especially when the various components of the environment are periodic with not necessarily commensurate periods.
