Das Projekt "Wind Tunnel study of sheltering effect by vegetation in the atmospheric boundary layer: implication for soil erosion and snow transport" wird vom Umweltbundesamt gefördert und von Eidgenössische Forschungsanstalt für Wald, Schnee und Landschaft, Eidgenössisches Institut für Schnee- und Lawinenforschung durchgeführt. Soil erosion and desertification, blowing and drifting snow, transport of pollen and seeds, dust entrainment and transport of (particulate) pollutants are some among a large number of processes governed by wind blowing on an erodible surface. The impact of these processes on the environment and both directly and indirectly on the human societies is huge, having implications for land surface geomorphology, human health, water resources, soil fertility and ecosystem biogeochemistry. In order to have full understanding of the physical mechanisms responsible for soil/snow entrainment, it is thus of crucial importance to investigate the very inner layer of the atmosphere, as close as possible to the ground. The interaction between the wind and the earth surface gives rise to a turbulent boundary layer which can lead to erosion of particles, often ranging from micron sized dust to millimeter sand grains. The action of the turbulent boundary layer essentially lead to a stress acting on the surface and ultimately a force acting on each single particle. In fluid mechanics the latter is referred to as the shear stress. In all surface transport models (from dust in deserts, to gravel in rivers, to PM10 particles in an industrial area) the shear stress is the key parameter. The amount of particles transported has almost always been described as a function of the difference between the shear stress and a threshold. Therefore, the prediction of the shear stress acting on the surface is a crucial pre-requisite to estimate mass transport rates. Very often, erodible soil or snow surfaces are covered by vegetation. It has long been known that vegetated surfaces prevent soil erosion by means of mainly three mechanisms. Firstly vegetation shelters the soil by simply reducing the surface exposed to the wind. Secondly, vegetation can trap particles in motion hence acting like a sink for sediments. Finally, vegetation decreases the shear stress acting on the erodible ground by absorbing the momentum flux from the airflow above, therefore weakening the erosive power of the wind. In this project we are concerned with quantifying this last effect for a selected variety of plants species and plant cover densities. The long term application of such study will be to develop a model which, for a given wind velocity and vegetation cover is able to predict the shear stress acting on the bottom surface. Such information can then be used as an input for sediment/snow transport models.