Ozone occurs at all levels of the earth's atmosphere. The density of ozone varies both seasonally and latitudinally. At Edmonton, Canada, the density $D(h)$ of ozone $\left(\text { in } 10^{-3} \mathrm{cm} / \mathrm{km}\right)$ for altitudes $h$ between $20 \mathrm{kllo}$ meters and 35 kilometers was determined experimentally. For each $D(h)$ and season, approximate the altitude at which the density of ozone is greatest.
$$D(h)=-0.058 h^{2}+2.867 h-24.239 \text { (autumn) }$$