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Lithofacies and depth are the main controls on permeability, and so lithofacies distribution exerts a key control on hydraulic behaviour.
Antecedent streamflow cumulated from the beginning of the wateryear was found to be the strongest predictor of baseflow recession rates, indicating that inter-seasonal differences in aquifer storage are a key control on baseflow recession rates in California watersheds.
The size of sediments entering channels is a key control on river morphodynamics across a range of scales, from channel response to human land use to landscape response to changes in tectonic and climatic forcing.
In contrast with the lower Gangetic plain, where large-scale floodplain sedimentary features are a key control on solid-phase As and Fe speciation, in these alluvial sediments solid-phase As and Fe speciation appears to be controlled mainly by physiographic properties (elevation; depth; seasonal water table) that influence local redox conditions.
In turn, moisture in walls provides a key control on decay processes [29].
Frictional properties of a fault, particularly at coseismic slip velocities, are a key control on whether an earthquake rupture can propagate up-dip through subduction forearcs (e.g., Faulkner et al. 2011).
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Most recently, Houthi rebels in northern Yemen seized a key control post on a strategic highway linking the capital San'a with Saudi Arabia, overcoming an army brigade after 12 hours of intense combat.
Alternatively, you can hold the Command key (control on windows) and press Up-Arrow.
A method was developed whereby in-river and riverbank electrical resistivity surveys were used to map the spatial coverage and thickness of the riverbed clay layer, thought to be the key control on infiltration in this environment.
Rock type variation is interpreted to be the key control on morphometric indices within the Gouritz catchment, especially hypsometry and stream length gradient.
A sensitivity analysis of key controls on water surface elevation and final sediment thickness illustrates how the flow was supply-limited in the upper reaches.
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