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we decrease » _ decrease (Expand Search)
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a decrease » _ decrease (Expand Search), _ decreased (Expand Search), _ decreases (Expand Search)
2 we » _ we (Expand Search), 2 de (Expand Search), 2 e (Expand Search)
we decrease » _ decrease (Expand Search)
nn decrease » _ decrease (Expand Search)
a decrease » _ decrease (Expand Search), _ decreased (Expand Search), _ decreases (Expand Search)
2 we » _ we (Expand Search), 2 de (Expand Search), 2 e (Expand Search)
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Convection In A Rotating Fluid Over A Sloping Bottom, With Application To The Arabian Gulf
Published 1992“…The results of the two dimensional model are presented herein. These results include (i) a detailed description of the evapora-tive-convective adjustment process; (ii) a measure of the convective length scale and vertical velocity; (iii) an assessment of the relative strengths of the buoyancy induced geostrophic current in the alongshore direction and the direct wind induced velocities; (iv) an assessment of the effect of wind on the density structures and (v) an analogy between the forcing by diffusive buoyant source and advective buoyant source.…”
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788
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Basin of Attraction through Invariant Curves and Dominant Functions
Published 2015“…We study a second-order difference equation of the form z<inf>n+1</inf> = z<inf>n</inf> F (z<inf>n-1</inf>) + h, where both F (z) and z F (z) are decreasing. …”
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793
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800