Cute Young Dark Blonde Girl Reveals In White Shorts On The Shore With Saltating Sands During Low Tide

At higher speeds, the lift and moment exerted by the fluid on the particle is enough to pull it away from the surface and into the flow. Initially the particle moves quite rapidly compared to the flow and so has high lift, moving it away from the surface. As the particle moves into the faster flow away from the bed, the velocity difference between particle and flow decreases, and so lift decreases. When the particle weight is greater than the lift force, the particle sinks back towards the surface. During its descent, the particle keeps some of the speed it picked up in the faster moving flow, and so returns to the surface at higher speed than the fluid near the surface.
Depending on the surface, more loose material could be dislodged by the impacting particle, the particle might disintegrate on impact, or the particle could continue bouncing downstream. In rivers, this process repeats continually, gradually eroding away the river bed, but also transporting-in fresh material from upstream.
Suspension generally affects small particles ('small' means 100 micrometres or less for particles in air). These particles experience lift forces which are similar in magnitude to the weight of the particle. These smaller particles are carried by the fluid in suspension, and convected downstream. Particles are carried until the fluid decelerates. When the weight is greater than the lift, the particles settle out.
A recent study finds that saltating sand particles induces a static electric field by friction. Saltating sand acquires a negative charge relative to the ground which in turn loosens more sand particles which then begin saltating. This process has been found to double the number of particles predicted by previous theory. This is significant in meteorology because it is primarily the saltation of sand particles which dislodges smaller dust particles into the atmosphere. Dust particles and other aerosols such as soot affect the amount of sunlight received by the atmosphere and earth, and are nuclei for condensation of the water vapour.