Exact(5)
Here is a sampling of some of the issues addressed using solid mechanics concepts: How do flows develop in the Earth's mantle and cause continents to move and ocean floors to subduct (i.e., be thrust) slowly beneath them?
Vortical flows develop at very low angles of attack, and form close to the wing surface.
Three-dimensional (3D) convection flows develop, which in turn affect the heat transfer process and hence the temperature pattern.
These basin flows develop biotic and non-biotic components that flourish, coordinate, and diversify ecological systems which support local croplands, forests, wetlands, vegetation, lakes, and communities.
Flash floods and debris flows develop at space and time scales that conventional observation systems for rainfall, streamflow and sediment discharge are not able to monitor.
Similar(55)
Here, we will just present this extra convexity assumption, needed for the existence of EVI gradient flows developed in [3].
The pulsation-free flows developed in two nanopumps push out the solutions contained in two reservoirs.
An inverse type of flow develops in the summer as the continents heat more rapidly than their adjacent oceanic areas.
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Such a flow develops after a short lag and follows the same pattern as the return of field lines drawn away from the Sun by viscous interaction.
As the winds travel from areas of higher pressure to areas of lower pressure, a persistent onshore flow develops over large landmasses in the lower troposphere.
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