Collectively, our results are consistent with the hypothesis that a major fraction of the changes in expression induced after miR-7 or miR-128 transfection are likely the indirect or down-stream consequences of changes in hub gene expression.
Although this phenomenon may reduce the effect of land use change on peak discharge in a large river basin, a sub-watershed (or micro catchment) may experience overall increase in peak stream flow as a result of changes in land use (Brooks et al. [1991]; Bruijnzeel [1990]; FAO, CIFOR [2005]).
The addition of various kinds of pollutants through sewage, industrial effluents, agricultural runoff, etc., into the water main stream brings about a series of changes in the physicochemical characteristics of the water, which have been the subject of several investigations (Bernard and Ayeni 2012).
For example, it is still an open question whether a loss of summer arctic ice is, by way of changes in the jet stream, responsible for unusual weather in mid latitudes, such as last month's frigid American "Polar Vortex" or Britain's recent floods.
Although the points of runoff against temperatures are highly scattered, there exists decreasing trends of runoff with temperature rise for all three phases, showing discharges are weakly correlated to temperature (linear correlation coefficients ranging from 0.012 to 0.179) and implying temperature is but not a dominant driver of change in stream flow.
We analyzed spatial patterns of thermal sensitivity (response of stream temperature to changes in air temperature) and maximum stream temperature for 74 stations in the Columbia River basin, to identify landscape factors affecting these two indices of stream temperature regimes.
Within the politics stream, these changes in jurisdiction altered positions of power and shifted priorities on the agenda.
The spatial distribution of lineaments expresses itself in terms of topography in the study area, which manifested as straight stream valley, sudden changes in flow direction of drainage patterns, contrasting tone, straight/curvilinear ridges and alignment of vegetation (Mabee et al. 1994; Masoud and Koike 2006; Ekwe et al. 2010; Adiat et al. 2012; Akinluyi 2013; Dasho et al. 2017).
Scientists are making much of the jet stream and how changes in these strong winds are affecting the weather.
Much has been made of the jet stream and how changes in these strong winds affect our weather.
