Longer dry periods can reduce vegetation cover and leave soil exposed. High temperatures accelerate moisture loss and increase plant stress. When intense rainfall follows drought, dry or sealed surfaces may absorb water too slowly, producing rapid runoff and erosion. Repeated freeze–thaw cycles create a different form of stress by disrupting soil structure and weakening newly established vegetation.
Climate adaptation does not mean designing around a single forecast or extreme event. It requires identifying which environmental stresses are relevant to the site and how they may interact over the expected life of the surface.
The objective is to develop systems that can maintain essential functions—such as erosion resistance, infiltration, moisture availability and vegetation cover—across a wider range of conditions.

