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  • Predicting wind velocities from sand dune and draa spacings determined by Fourier analysis in Interpretation of windflow characteristics from Eolian landforms.
  • The spacing of sand dunes and draas (dune groups) is one parameter that can be used to estimate wind velocity and available wind power. Measurements of spacings can be made directly from LANDSAT imagery or aerial photography. Fourier analysis
  • of these measurements reveals the predominant spacings. Assuming that shear velocity is the dominant factor determining the wave leugth of bedforms, the spacing can be used to compute the threshold shear velocity using mathematical relationships derived by Wilson (1972
  • 1982
  • A study of space variations of precipitation by factor analysis
  • 1982
  • Population regionals a perspective in geographic space of India in Natural hazards management in South America.
  • 1982
  • Dynamic plant ecology: the spectrum of vegetational change in space and time
  • 1982
  • Space-time quantification of rainfall inputs for hydrological transport models
  • 1982
  • Bed forms and bend-arc spacings of some coarse bedload channels in upland Britain
  • 1982
  • The A. examines the original approaches made by the geographers of the French Regional School to the study of climate, the critique of data, the transition from the research station network to regional space, the recourse to field observations
  • 1982
  • Spatial variations in dune height and spacing and in the grain size and sorting parameters of dune crest sands suggest that the Namib sand sea has accumulated principally by the movement of sands from southern and western coastal source areas
  • 1982
  • Comparative ecological analyses of the species diversity of old tropical rain forest ecosystems show that their biocenoses are the more likely to have both low fluctuations and low resilience the more homogeneous the environment in space and time
  • 1982
  • of space and seasonal variability analysis of these characteristics are given. Specific features of the structure of their variations described with the help of a polynomial trend are considered. (Ed.).
  • 1982