DREB is a well-known transcription factor that is induced by drought and it activates many down stream stress-responsive genes to ultimately improve the drought and chilling tolerance of rice [ 36].
These variables can create a constant stream of stress.
Then it started constantly happening, across cities and countries all over Europe causing a consistent stream of stress and confusion.
Among the five hydraulic factors (i.e., flow velocity, runoff depth, shear stress, stream power, and unit stream power), flow velocity and stream power showed close relationships with SOC concentration, especially the average flow velocity at 2 m from the outlet where the runoff attained the maximum sediment load.
The objectives of this study were to evaluate the effects of flow discharge (Q), slope gradient (S), flow velocity (V), shear stress, stream power and unit stream power (U) on sediment concentration.
The relationship of sheet erosion rate (SE), slope gradient (S) and rainfall intensity (I), and hydraulic parameters, such as flow velocity (V), shear stress, stream power and unit stream power (P), was investigated to derive an accurate experimental model.
With this background, CBE can be understood as a consequence of cellular imperatives in which self-referential cells sustain homeostatic preferences in the face of a stream of stresses as biological ambiguities.
The relationship between soil detachment capacity (Dc) by rill flow and hydraulic parameters (e.g., flow velocity, shear stress, unit stream power, stream power, and unit energy) at low flow rates is investigated to establish an accurate experimental model.
GIS-based implementations of the shear stress, stream power per unit length and stream power per unit area models are closely related to one another and related also to empirical sediment yield models derived from continental-scale factor analyses.
This apparent contradiction is explained through an analysis of temporal adjustments to flow energy, shear stress, and stream power with time.
