Green roofs provide a vegetated layer that can capture and temporarily store stormβwater, reducing peak runoff rates and mitigating downstream flooding. The amount of water retained depends primarily on the roofβs surface area, the depth of the growing substrate, and the substrateβs porosity, which determines how much void space is available for water storage.
When a rain event occurs, the volume of water that reaches the roof is the product of the roof area and the rainfall depth. The substrate can absorb water up to its storage capacity, which is calculated from its physical depth and the fraction of that depth that is void space (porosity). Any excess water beyond this capacity will flow off the roof as runoff.
Designers use these relationships to size greenβroof systems for a target storm event, ensuring that the retained volume meets regulatory or siteβspecific stormwater management goals while also providing ancillary benefits such as insulation and habitat.
A = roof area (mΒ²)
d = substrate depth (m)
n = substrate porosity (fraction)
How does rainfall depth affect water retention on a green roof?
What role does substrate porosity play in green roof water retention?
How can I increase the water retention capacity of my green roof?
What is the formula for calculating water retention on a green roof?
How does the surface area of the roof impact water retention?
Can green roofs help mitigate flooding in urban areas?
What are the benefits of using a green roof for water retention?
Results are for informational purposes only and do not constitute professional advice.
