Hydrological Cycle
The hydrological cycle, also known as the water cycle, represents the continuous movement of water within the Earth's hydrosphere in different states: liquid, solid, and gas. This cycle includes various processes such as evaporation, condensation, precipitation, and runoff.
Key Components of the Hydrological Cycle:
- Evaporation: Water from oceans and land surfaces transitions to vapor.
- Condensation: Water vapor cools and forms droplets, contributing to cloud formation.
- Precipitation: Water returns to the surface as rain, snow, etc.
- Runoff and Infiltration: Water flows over land and infiltrates the ground, returning to rivers, lakes, and aquifers.
About 71% of the Earth's surface is covered by water, with the majority found in oceans. Freshwater sources, such as glaciers, groundwater, and lakes, constitute a small percentage of the total water supply.
Due to pollution and increasing demand for water, many regions face water scarcity challenges.
Through the study of the hydrological cycle, we understand its crucial role in supporting ecosystems and human life, emphasizing the importance of sustainable water management.