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Water cycle

earth science Maturity 9-11 Next article →

The water cycle, also known as the hydrologic cycle, is a continuous biogeochemical cycle. It involves the constant change in the form of water on, above, and below the Earth's surface. This cycle moves water between different reservoirs through various physical and chemical processes. While water moves constantly, the total mass of water on Earth remains fairly constant over time. However, how that water is partitioned into ice, fresh water, salt water, and atmospheric water can change based on climate.

HydrologicalCycle1
HydrologicalCycle1

The entire cycle is powered by energy from the sun. This energy drives several different processes that move water between states. First, solar radiation heats water in oceans, lakes, and rivers. This causes evaporation, where liquid water transforms into a gas called water vapor. The ocean is a massive driver of this process, providing 86% of all global evaporation. Another process is transpiration, which is the release of water vapor from plants and soil. When these two processes happen together, it is called evapotranspiration. Additionally, snow and ice can turn directly into gas through a process called sublimation.

As water vapor rises into the atmosphere, it undergoes a change due to physics. Water molecules have a smaller molecular mass than the main gases in our air, like nitrogen and oxygen. This lower density creates buoyancy, which helps drive the vapor higher into the atmosphere. As the vapor reaches higher altitudes, the air pressure decreases and the temperature drops. This cooling forces the water vapor to undergo condensation, turning it back into liquid droplets. These droplets are supported by updrafts to form clouds. If this condensation happens very close to the ground, it is known as fog.

Once cloud particles collide and grow, they fall to the Earth as precipitation. This can take many forms, including rain, snow, hail, sleet, or graupel. About 78% of all global precipitation occurs over the ocean. When precipitation hits land, it moves through several pathways. Much of it flows over the ground as surface runoff, eventually entering rivers and streams. Other water moves through infiltration, where it soaks into the ground. This water can replenish aquifers, which are deep underground layers that store freshwater. Some water stays near the surface as soil moisture before moving into larger bodies of water.

USGS WaterCycle English ONLINE 20221013
USGS WaterCycle English ONLINE 20221013

Water spends different amounts of time in these reservoirs, a concept known as residence time. This is a measure of the average age of the water in a specific area. For instance, water in the atmosphere has a very short residence time of about 9 days. Rivers hold water for only 2 to 6 months on average. In contrast, deep groundwater can remain in aquifers for 10,000 years, often called fossil water. The largest storehouse is the ocean, which holds approximately 97% of the planet's total water. The Earth's ice caps and glaciers also act as major reservoirs, storing about 1.7% of all water.

HumanIntegratedWaterCycle (2)
HumanIntegratedWaterCycle (2)

The water cycle does more than just move moisture; it shapes our entire planet. As liquid water flows, it transports minerals across the globe. It also reshapes geological features through weathering, erosion, and deposition. The cycle also acts as a natural purification system. During evaporation, water molecules separate from the salts and particles present in the liquid. Furthermore, the cycle helps regulate temperature. The ocean moves heat from the tropics toward the poles through ocean circulation. This movement of heat is a critical part of the Earth's climate system.

Human activities are now significantly altering these natural patterns. Changes in land use, such as deforestation and urbanization, affect how water moves across the landscape. Building cities creates impervious surfaces that change how much water can soak into the ground. Additionally, climate change is causing an intensification of the water cycle. Global warming is shifting precipitation patterns and increasing the frequency of extreme weather events. These changes impact everything from agriculture and water availability to entire ecosystems and human societies.

Soil moisture and climate change
Soil moisture and climate change
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File:USGS WaterCycle English ONLINE 20221013.png
USGS WaterCycle English ONLINE 20221013.png
Earth's Water Cycle.ogv
File:HydrologicalCycle1.png
HydrologicalCycle1.png
File:HumanIntegratedWaterCycle (2).jpg
HumanIntegratedWaterCycle (2).jpg
File:Natural & impervious cover diagrams EPA.jpg
Natural & impervious cover diagrams EPA.jpg
File:20211109_Frequency_of_extreme_weather_for_different_degrees_of_global_warming_-_bar_chart_IPCC_AR6_WG1_SPM.svg
20211109_Frequency_of_extreme_weather_for_...
File:Soil_moisture_and_climate_change.svg
Soil_moisture_and_climate_change.svg
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