THE TOWER SHADOW EFFECT
暂无分享,去创建一个
Abstract : A practical example of obstacle-induced flow in the atmosphere that constitutes a substantial meteorological measurement problem is the 'wind shadow' effect of a meteorological tower on wind velocity in the lee of the structure. At White Sands Missile Range, New Mexico, a 150-meter tower is utilized to obtain ballistic winds in the lower portion of the planetary boundary layer. An experiment has been conducted concerning the flow around a 1:4 scale model section of the tower in the subsonic wind tunnel at the Fluid Dynamics Laboratory, Colorado State University, Ft. Collins, Colorado. Comparison of field results and experiment suggests a maximum wind decrement of 40% in the tower wake. (Author)
[1] C. W. Thornthwaite,et al. Disturbance of airflow around Argus Island tower near Bermuda , 1965 .
[2] D. Camp. Analysis of wind tunnel data for several beckman and whitley series 50 and climet model c1-14 anemometers , 1965 .
[3] Roy I. Glass. missile meteorology tower , 1964 .
[4] H. G. Daubek,et al. Errors in Wind Measurements Associated with Tower-Mounted Anemometers , 1961 .
[5] N. Tsuda,et al. What Are We Measuring on the Top of a Tower , 1957 .