The water cycle is the continuous movement of water in and around the Earth. Water never really goes away –it just changes form. The sun drives the entire water cycle and is responsible for its two major components: condensation and evaporation. When the sun heats the surface of water, it evaporates and ends up in the atmosphere as water vapor. It cools and rises, becoming clouds, which eventually condense into water droplets. Depending on the temperature of the atmosphere and other conditions, the water precipitates as rain, sleet, hail or snow.
Some of this precipitation is captured by tree canopies and evaporates again into the atmosphere. The precipitation that hits the ground becomes runoff, which can accumulate and freeze into snow caps or glaciers. It can also infiltrate the ground and accumulate, eventually storing in aquifers. An aquifer is a large deposit of groundwater that can be extracted and used. This runoff also comes from snowmelt, which occurs when the sun and climate changes melt snow and ice. Finally, some of this runoff makes its way back into lakes and oceans, where it is again evaporated.
Water that falls to the ground and stays in the soil ends up evaporating and retiring to the atmosphere. But groundwater, the major source of our drinking water, can accumulate in aquifers over thousands of years. Unconfined aquifers have the water table, or the surface where water pressure equals atmospheric pressure, as their upper boundaries. Confined aquifers often lie below unconfined aquifers and have a layer of rock or other materials as their top.
In the US, the oldest groundwater, known as fossil water, is contained in the Ogallala Aquifer. Lying below about 175,000 square miles of eight states in the Great Plains, the Ogallala Aquifer stores about 2,900 million acre-feet (3,600 million kilometers cubed) of water. The Ogallala Aquifer was formed between 2 and 6 million years ago, when the Rocky Mountain chain was forming. Because the climate of the Great Plains is arid, water in the aquifer is being used faster than it can be recharged. Thatâ€™s why some scientists refer to using fossil water aquifers as water mining.
Groundwater may also exist on other planets. Images from the Mars Global Surveyor spacecraft show what looked like gullies carved out by rivers of water on the surface of the planet. According to NASA, the water is probably 300 to 1,300 feet (100 to 400 meters) below the surface. Europa, one of Jupiterâ€™s moons, may also have subsurface water. As our need for water outweighs the Earthâ€™s supply, scientists wonder if we may one day mine for water on the other planets and moons in our solar system.
Water has a lot of unique and amazing properties that make it so important to life. Theyâ€™re why weâ€™re constantly looking for better ways to obtain and conserve it. In the next section, weâ€™ll look at these properties and learn more about water itself.