用英语写一个水的报告,不要太长.写水由天上的雨落在地下而形成水，而地下的水流进湖泊，之后湖泊的水变成水蒸气，在天上形成云，云又降水。（循环）

用英语写一个水的报告,不要太长.写水由天上的雨落在地下而形成水，而地下的水流进湖泊，之后湖泊的水变成水蒸气，在天上形成云，云又降水。（循环）
用英语写一个水的报告,不要太长.
写水由天上的雨落在地下而形成水，而地下的水流进湖泊，之后湖泊的水变成水蒸气，在天上形成云，云又降水。（循环）

用英语写一个水的报告,不要太长.写水由天上的雨落在地下而形成水，而地下的水流进湖泊，之后湖泊的水变成水蒸气，在天上形成云，云又降水。（循环）
太笼统了.水的报告是怎样的?有什么格式?题目是关于水污染的还是水再利用?
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Water cycle
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The water cycle.The water cycle, also known as the hydrologic cycle or H2O cycle, describes the continuous movement of water on, above and below the surface of the Earth. Water can change states among liquid, vapor, and ice at various places in the water cycle. Although the balance of water on Earth remains fairly constant over time, individual water molecules can come and go. Over geologic time, water-rich planets such as the Earth lose gases such as Hydrogen over time, which can lead to run away greenhouse effects which in turn accelerate Hydrogen loss, and by association water loss, from a planet's atmosphere.
Contents
1 Description
1.1 Different Processes
2 Residence times
3 Changes over time
4 Effects on climate
5 Effects on biogeochemical cycling
6 Slow loss over geologic time
7 See also
8 Notes
9 External links

Description
The sun, which drives the water cycle, heats water in oceans and seas. Water evaporates as water vapor into the air. Ice and snow can sublimate directly into water vapor. Evapotranspiration is water transpired from plants and evaporated from the soil. Rising air currents take the vapor up into the atmosphere where cooler temperatures cause it to condense into clouds. Air currents move water vapor around the globe, cloud particles collide, grow, and fall out of the sky as precipitation. Some precipitation falls as snow or hail, and can accumulate as ice caps and glaciers, which can store frozen water for thousands of years. Snowpacks can thaw and melt, and the melted water flows over land as snowmelt. Most water falls back into the oceans or onto land as rain, where the water flows over the ground as surface runoff. A portion of runoff enters rivers in valleys in the landscape, with streamflow moving water towards the oceans. Runoff and groundwater are stored as freshwater in lakes. Not all runoff flows into rivers, much of it soaks into the ground as infiltration. Some water infiltrates deep into the ground and replenishes aquifers, which store freshwater for long periods of time. Some infiltration stays close to the land surface and can seep back into surface-water bodies (and the ocean) as groundwater discharge. Some groundwater finds openings in the land surface and comes out as freshwater springs. Over time, the water returns to the ocean, where our water cycle started.
Different Processes
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.[1] Approximately 505,000 km3 (121,000 cu mi) of water fall as precipitation each year, 398,000 km3 (95,000 cu mi) of it over the oceans.[2]
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 both surface runoff 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 or groundwater.[3]
Subsurface Flow
The flow of water underground, in the vadose zone 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.[4] The source of energy for evaporation is primarily solar radiation. Evaporation often implicitly includes transpiration from plants, though together they are specifically referred to as evapotranspiration. Total annual evapotranspiration amounts to approximately 505,000 km3 (121,000 cu mi) of water, 434,000 km3 (104,000 cu mi) of which evaporates from the oceans.[2]
Sublimation
The state change directly from solid water (snow or ice) to water vapor.[5]
Advection
The movement of water — in solid, liquid, or vapor states — through the atmosphere. Without advection, water that evaporated over the oceans could not precipitate over land.[6]
Condensation
The transformation of water vapor to liquid water droplets in the air, creating clouds and fog.[7]
Transpiration
The release of water vapor from plants and soil into the air. Water vapor is a gas that cannot be seen.