air
Air
evaporation and transpiration
Some water returns to the atmosphere through evaporation or plants.
ONE CITY, ONE STORM
When rain hits a city, the surface beneath it chooses the first route. Follow one drop and watch asphalt, soil, plants, a tank and a pipe divide the same water.
Original illustration. An urban cutaway with simplified proportions, drawn for explanation.
THE FIRST TOUCH
Across 100 m², 30 mm of rain equals exactly 3,000 litres. The water reaches the same city, but the first surface it touches changes its speed, filter and next destination.
Calculation: 30 mm × 100 m² = 3,000 L. The volume is exact under this assumption. The split below is modeled.
FOLLOW THE DROP
Choose the rainfall, then send one drop through the city cutaway. In a large storm, soil and storage take less while pipe and river take more.
Routes in the illustration
The drop is waiting at the edge of the roof.
of volume, in model
Without JavaScript, the cutaway remains a static map of the five routes. The initial values describe the 30 mm scenario.
FIVE ROUTES
Use these five routes as a working map. One drop can pass through several over time. The model follows the destination that appears first for each portion of water.
air
evaporation and transpiration
Some water returns to the atmosphere through evaporation or plants.
soil
infiltration
Water enters the ground. Speed depends on pores, compaction, slope and what is already there.
tank
retention and reuse
A roof, barrel or planted hollow can hold water long enough to release it slowly.
pipe
fast conveyance
Impervious surfaces send water quickly toward gutters, drains and pipes.
river
surface runoff
Water that leaves over the surface can carry sediment, nutrients and metals with it.
ASPHALT AND PIPE
Street, parking lot and roof do not let water enter soil easily. Rain moves fast, picks up sediment and other substances from the surface, then enters drains or reaches surface water.
Documented fact
The EPA describes runoff from streets, parking lots and roofs as a route that can carry trash, bacteria, nutrients, sediment and metals into water.
What the model shows
In the model, pipe and river grow when the surface becomes compact and rain arrives faster than water can enter the soil.
Source for this distinction ↗WHAT SLOWS THE WATER
Rain gardens, permeable pavement, green roofs and storage tanks put distance between a drop and a pipe. They can store, filter, infiltrate or evapotranspirate water when the site and maintenance allow it.
A rain garden cannot fix every street. The EPA ties the result to site, soil, design and maintenance.
holds water in a planted hollow and lets it pass through soil
lets water reach gravel and soil layers below
holds some rain and releases it more slowly
keeps water for later use or slower release
AFTER THE STORM
Before asking how large the pipe should be, look at which water reaches it and how fast. A storm is not one event. It is a sequence of surfaces and routes.
When the next storm arrives, look first at the place where water meets the ground.
SOURCES AND MODEL
The sources below support the hydrologic mechanisms and infrastructure described on the page. The 3,000-litre figure is a direct calculation. The percentages splitting water across five routes are an editorial model, used to make the shift between a small and a large storm visible.
Explains evaporation, infiltration and runoff as parts of the water cycle.
Scope: General hydrologic principles; it does not supply the coefficients used in the interactive model.
Open sourceDefines infiltration, filtration and evapotranspiration and describes the difference between impervious surfaces and systems that manage water where it falls.
Scope: Definitions and mechanisms; examples come from EPA guidance, not a local measurement.
Open sourceShows how rain from streets, parking lots and roofs picks up pollutants and reaches drains or surface waters.
Scope: General explanation of urban runoff and green solutions.
Open sourceDescribes rain gardens, permeable pavements, green roofs, planters and rain barrels.
Scope: Intervention types and possible functions: retention, filtration, infiltration and evapotranspiration.
Open sourceConnects the volume of water entering pipes with localized flooding risk and water quality.
Scope: System-level benefits and limits; exact effects depend on site and design.
Open sourceDescribes wet-weather flow, retention basins and discharge toward the Dâmbovița in documentation for Bucharest’s treatment plant.
Scope: Local institutional and technical context; this page does not transfer the document’s flows into the 100 m² model.
Open source| Storm | Total volume | Modeled split |
|---|---|---|
| 5 mm | 500 L | Air: 11% · Soil: 43% · Storage: 22% · Pipe: 19% · River: 5% |
| 30 mm | 3,000 L | Air: 7% · Soil: 27% · Storage: 12% · Pipe: 38% · River: 16% |
| 60 mm | 6,000 L | Air: 4% · Soil: 15% · Storage: 6% · Pipe: 43% · River: 32% |