Suspension transport of wind‐eroded sand particles

Abstract

Sand‐sized particles occupy the region 0 S x, z 0, c(x, z) decays with z on a length scale (i.e. a unit of distance) which depends on m and not on 0. For fixed z, on the other hand, c(x, z) decays on a horizontal length scale X which depends on p and m as well as on the friction velocity. The concentration decays algebraically to zero as X tends to infinity. Copyright © 1991, Wiley Blackwell. All rights reserved