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During the E-wave downstroke, the strongly adverse gradient embodies the streamwise pressure augmentations from both local and convective decelerations.
The flow for α < 90° is a favorable gradient and never separates, the expanding area produces, α > 90°, low velocity and increasing pressure, an adverse gradient.
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Adverse gradients that exceed 11 times that of the ice surface may even permit the formation of subglacial lakes.
Subglacial basins are important glaciologically because they require ice, water and sediment to ascend an adverse subglacial slope in order to exit the glacial system, the efficiency of which is dependent upon the gradient of the adverse slope and that of the ice surface.
The variable φ, an anisotropy parameter of the Reynolds stresses, decreases due to the deceleration effect through an adverse pressure gradient, and increases due to the acceleration effect through a favorable pressure gradient.
He could pull out the three-view drawing of the land-based aircraft he designed for antisubmarine warfare or talk about adverse pressure gradient.
Boundary layer separation initiated by the adverse pressure gradient is identified using Large Eddy Simulation.
There is no adverse pressure gradient against which the material has to be fed.
This is ascribed to the adverse pressure gradient strength and the potential core-like region extension.
The comparative studies cover the controlling of low-speed separated flows in adverse pressure gradient and supersonic shock-induced separation.
This type of flow is characterized by the presence of an adverse pressure gradient along the airfoil chord.
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