2 Atmospheric drag and the atmosphere. The effect of the atmosphere on the surface drag has been investigated experimentally using the Reynolds number. The analysis involved the evaluation of the coefficients of drag, and the evaluation of the coefficients of surface area, volume, pressure, pressure at sea level (at the Earth's surface), and the corresponding atmospheric drag. The surface drag coefficient of the atmosphere and its surface area determined for a simple atmosphere consist of three quantities, namely the drag factor, the pressure difference between the source-air and the target-air regions, and the pressure difference between the source-air and the atmospheric layer with a distance of about 2.5 cm. The atmospheric drag is assumed to be uniform and to vary linearly with the square of the height (i.e., v/h): This results in a variation of the atmosphere-surface drag coefficient with height of 2 /\ (v / h). The analysis shows that, if we assume an atmospheric pressure of 1 tour which differs from the surface pressure by the pressure differential over the atmosphere, the atmosphere-surface drag value for the atmosphere varies with height by a fixed factor 1/(2/2) (where is the surface roughness constant). The surface drag with the atmosphere has the form of: The surface-air and the atmospheric-layer values are the same at the same height but differ by a factor of 1/(2/2). This means: The surface-air and the atmospheric-layer values should be measured at the same point over such a region of the Earth. Using the results to show that the atmosphere produces a drag-on effect on the surface which depends on height above the surface, we see how well it predicts the experimental results for surface drag calculations. The values of the atmospheric drag for different heights result in an increase as the height increases and the height-gradient of the atmosphere is obtained; these are summarized and compared. 12.3.1.2.1. Effects of height from the atmosphere. Assuming a vertical and a lateral drag coefficient (d.d.c and d.d.c.) of 0.2, the average surface surface-drag coefficient per unit volume is given by d = 0.00057, where the drag coefficient in the horizontal direction of the atmosphere is given by d (r). This means that the drag is proportional to density of the atmospheric layer and proportional, at most, to the atmospheric thickness.
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(Manuscript received 4 February 2000, in final form 22 August 2000). ABSTRACT ...... 12d mark the local maxima and minima in time of the surface drag for. 7.5.
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I-010 Form 1 Wisconsin is a tax form used to report income and calculate state taxes owed by individuals in the state of Wisconsin.
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