Britannica AI Icon

residence time

hydrologic cycle

Quick Summary

The hydrologic cycle, or water cycle, describes the continuous circulation of water between the Earth and its atmosphere. Key processes include evaporation, transpiration, condensation, precipitation, and runoff.

The residence time of water varies significantly across different reservoirs. For instance, water in the oceans can remain for over 3,000 years, while water in the atmosphere typically stays for only about 10 days before returning to Earth as precipitation. Water in lakes, rivers, ice, and groundwater has variable residence times between these extremes.12

Summary created from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles.

Ask Britannica AI about this topic

Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.