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  • of data gathered and gives examples of how the data are being used both for environmental reporting and research into aeolian processes and activity.
  • and ejected velocities gained by the three-dimensional model are lower than the corresponding ones done by two-dimensional model apart from the horizontal rebound velocity. It also shows the lateral velocity and the lateral angular velocity, as well
  • rotation periods, for which long-term climatic records (1961-2004) were used. High plant or residue soil coverage as well as high oriented surface roughness eliminated erosion according to WEPS and RWEQ. These results indicated that WEQ can be used
  • to agree well with the synoptic records and satellite images.