Kutzbach reports wind profiles over a series of roughness elements on a frozen lake and how the wind profile changed as the surface roughness was varied. The approach of the current study was to duplicate Kutzbach's roughness arrays in the wind tunnel at 1/20 and 1/40 scales, and to compare the wind profiles over these scale models to those derived by Kutzbach at full scale in the field. The effects of scale differences and data reduction techniques are discussed. Although the study suggests that wind tunnel scale models can predict parameters measured in the field, the development of more definitive guidelines requires a field experiment designed specifically for comparison with wind tunnel results
Aeolian processes are major determinants of geomorphology on bodies in the Solar System possessing a...
Wind is currently the dominant geological agent acting on the surface of Mars. A study of Martian ae...
The relation between wind, momentum flux, roughness and land-use in disturbed, non-homogeneous bound...
This study evaluates how well values of aerodynamic surface roughness, z sub 0, measured over scale ...
Eolian erosion and deposition on earth was studied in order to interpret the eolian land forms of Ma...
The physics and geological relationships of particles driven by the wind under near Martian conditio...
The characteristics of aerolian (wind) activity as a surface modifying process on Earth, Mars, Venus...
The objective of the research was to assess the significance of aeolian (windblown) processes in the...
Preliminary results are reported of an investigation which involves wind tunnel simulations, geologi...
Obtaining reliable estimates of aerodynamic roughness is necessary to interpret and accurately predi...
A laboratory facility proposed for the Space Station to investigate fundamental aspects of windblown...
International audienceMany boundary layer processes simulated within a Mars General Circulation Mode...
Global and regional patterns on Mars were inferred from surface aeolian features, such as wind strea...
This is the first analysis of the high frequency data from the Viking lander and spectra of wind, in...
Aerodynamic roughness heights of 1-3 cm were obtained from measured wind profiles collected among fi...
Aeolian processes are major determinants of geomorphology on bodies in the Solar System possessing a...
Wind is currently the dominant geological agent acting on the surface of Mars. A study of Martian ae...
The relation between wind, momentum flux, roughness and land-use in disturbed, non-homogeneous bound...
This study evaluates how well values of aerodynamic surface roughness, z sub 0, measured over scale ...
Eolian erosion and deposition on earth was studied in order to interpret the eolian land forms of Ma...
The physics and geological relationships of particles driven by the wind under near Martian conditio...
The characteristics of aerolian (wind) activity as a surface modifying process on Earth, Mars, Venus...
The objective of the research was to assess the significance of aeolian (windblown) processes in the...
Preliminary results are reported of an investigation which involves wind tunnel simulations, geologi...
Obtaining reliable estimates of aerodynamic roughness is necessary to interpret and accurately predi...
A laboratory facility proposed for the Space Station to investigate fundamental aspects of windblown...
International audienceMany boundary layer processes simulated within a Mars General Circulation Mode...
Global and regional patterns on Mars were inferred from surface aeolian features, such as wind strea...
This is the first analysis of the high frequency data from the Viking lander and spectra of wind, in...
Aerodynamic roughness heights of 1-3 cm were obtained from measured wind profiles collected among fi...
Aeolian processes are major determinants of geomorphology on bodies in the Solar System possessing a...
Wind is currently the dominant geological agent acting on the surface of Mars. A study of Martian ae...
The relation between wind, momentum flux, roughness and land-use in disturbed, non-homogeneous bound...