Hydrological cycle and runoff
The journey from raindrop to river runoff is what decides whether a storm becomes a flood. We explain the hydrological cycle step by step: precipitation, interception, infiltration, surface runoff, and channel flow, and why factors like soil moisture, slope, and urban impervious surfaces dramatically change a basin's response to heavy rain.
English version coming soon
Full English translation is in preparation. In the meantime, you can read the original Spanish version.
Read in Spanish →