The Water Cycle
Autor: Homem de Átomos | Publicado: 2011-09-13T14:33:00-07:00





Concepts:


The water cycle or hydrologic cycle&nbsp;is a continuous cycle where water evaporates, travels into the air and becomes part of a cloud, falls down to earth as precipitation, and then evaporates again. This repeats again and again in a never-ending cycle. Water keeps moving and changing from a solid to a liquid to a gas, over and over again. 



Precipitation creates runoff that travels over the ground surface and helps to fill lakes and rivers. It also percolates or moves downward through openings in the soil to replenish aquifers under the ground. Some places receive more precipitation than others do. These areas are usually close to oceans or large bodies of water that allow more water to evaporate and form clouds. Other areas receive less precipitation. Often these areas are far from water or near mountains. As clouds move up and over mountains, the water vapor condenses to form precipitation and freezes. Snow falls on the peaks.








The process:

Precipitation: Condensed water vapor that falls to the Earth's surface. Most precipitation occurs as rain, but also includes snow, hail, fog drip, graupel, and sleet.&nbsp;Approximately 505,000 km3 (121,000 cu&nbsp;mi) of water falls as precipitation each year, 398,000 km3 (95,000 cu&nbsp;mi) of it over the oceans.

Canopy interception: The precipitation that is intercepted by plant foliage and eventually evaporates back to the atmosphere rather than falling to the ground.

Snowmelt: The runoff produced by melting snow.

Runoff: The variety of ways by which water moves across the land. This includes bothsurface runoff&nbsp;and channel runoff. As it flows, the water may seep into the ground, evaporate into the air, become stored in lakes or reservoirs, or be extracted for agricultural or other human uses.

Infiltration: The flow of water from the ground surface into the ground. Once infiltrated, the water becomes soil moisture&nbsp;or groundwater.

Subsurface Flow: The flow of water underground, in the vadose zone&nbsp;and aquifers. Subsurface water may return to the surface (e.g. as a spring or by being pumped) or eventually seep into the oceans. Water returns to the land surface at lower elevation than where it infiltrated, under the force of gravity or gravity induced pressures. Groundwater tends to move slowly, and is replenished slowly, so it can remain in aquifers for thousands of years.

Evaporation: The transformation of water from liquid to gas phases as it moves from the ground or bodies of water into the overlying atmosphere. The source of energy for evaporation is primarily solar radiation. Evaporation often implicitly includes transpiracion from plants, though together they are specifically referred to as evapotranspiration. Total annual evapotranspiration amounts to approximately 505,000 km3 (121,000 cu&nbsp;mi) of water, 434,000 km3 (104,000 cu&nbsp;mi) of which evaporates from the oceans.

Sublimation: The state change directly from solid water (snow or ice) to water vapor.

Advection: The movement of water&nbsp;— in solid, liquid, or vapor states&nbsp;— through the atmosphere. Without advection, water that evaporated over the oceans could not precipitate over land.

Condensation: The transformation of water vapor to liquid water droplets in the air, creating clouds and fog.

Transpiration: The release of water vapor from plants and soil into the air. Water vapor is a gas that cannot be seen.



Experience: 76940