<P> The water cycle involves the exchange of energy, which leads to temperature changes . When water evaporates, it takes up energy from its surroundings and cools the environment . When it condenses, it releases energy and warms the environment . These heat exchanges influence climate . </P> <P> The evaporative phase of the cycle purifies water which then replenishes the land with freshwater . The flow of liquid water and ice transports minerals across the globe . It is also involved in reshaping the geological features of the Earth, through processes including erosion and sedimentation . The water cycle is also essential for the maintenance of most life and ecosystems on the planet . </P> <P> The sun, which drives the water cycle, heats water in oceans and seas . Water evaporates as water vapor into the air . Some ice and snow sublimates directly into water vapor . Evapotranspiration is water transpired from plants and evaporated from the soil . The water molecule H O has smaller molecular mass than the major components of the atmosphere, nitrogen and oxygen, N and O, hence is less dense . Due to the significant difference in density, buoyancy drives humid air higher . As altitude increases, air pressure decreases and the temperature drops (see Gas laws). The lower temperature causes water vapor to condense into tiny liquid water droplets which are heavier than the air, and fall unless supported by an updraft . A huge concentration of these droplets over a large space up in the atmosphere become visible as cloud . Some condensation is near ground level, and called fog . </P> <P> Atmospheric circulation moves water vapor around the globe, cloud particles collide, grow, and fall out of the upper atmospheric layers as precipitation . Some precipitation falls as snow or hail, sleet, and can accumulate as ice cap s and glacier s, which can store frozen water for thousands of years . 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 water emerging from the ground (groundwater) may be 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 can 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 . In river valleys and floodplains, there is often continuous water exchange between surface water and ground water in the hyporheic zone . Over time, the water returns to the ocean, to continue the water cycle . </P>

What two forces keep the water cycle going