An atmospheric boundary layer is formed when the wind blows over the Earth's surface. Typically, such velocity profiles can be written as a power law: $u=a y^{n},$ where the constants $a$ and $n$ depend on the roughness of the terrain. As is indicated in Fig. $P 9.22,$ typical values are $n=0.40$ for urban areas, $n=0.28$ for woodland or suburban areas, and $n=0.16$ for flat open country (Ref. 23).
(a) If the velocity is $20 \mathrm{ft} / \mathrm{s}$ at the bottom of the sail on your boat $(y=4 \mathrm{ft}),$ what is the velocity at the top of the mast $(y=30 \mathrm{ft}) ?(\mathrm{b})$ If the average velocity is $10 \mathrm{mph}$ on the tenth floor of an urban building, what is the average velocity on the sixtieth floor?