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  2. Water balance - Wikipedia

    en.wikipedia.org/wiki/Water_balance

    The law of water balance states that the inflows to any water system or area is equal to its outflows plus change in storage during a time interval. [ 2 ] [ 3 ] In hydrology , a water balance equation can be used to describe the flow of water in and out of a system.

  3. Ecohydrology - Wikipedia

    en.wikipedia.org/wiki/Ecohydrology

    The concept of water deficit, as developed by Stocker in the 1920s, [6] [7] [8] is a useful index of the balance in the plant between uptake and loss of water. Slight water deficits are normal and do not impair the functioning of the plant, [9] while greater deficits disrupt normal plant processes.

  4. Outline of hydrology - Wikipedia

    en.wikipedia.org/wiki/Outline_of_hydrology

    Designing sewers and urban drainage system; Determining the agricultural water balance; Determining the water balance of a region; Fog collection; Part of the hazard module in catastrophe modeling; Predicting and mitigating flood, landslide and drought risk; Predicting geomorphologic changes, such as erosion or sedimentation; Providing drinking ...

  5. The system that moves water around the Earth is off balance ...

    www.aol.com/news/global-water-cycle-off-balance...

    “The global water crisis is a tragedy but is also an opportunity to transform the economics of water,” said Ngozi Okonjo-Iweala, director general of the World Trade Organization and a co-chair ...

  6. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    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 the climate system. The evaporative phase of the cycle purifies water because it causes salts and other solids picked up during the cycle to be left behind.

  7. Groundwater recharge - Wikipedia

    en.wikipedia.org/wiki/Groundwater_recharge

    Water balance. Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table ...

  8. Environmental impact of reservoirs - Wikipedia

    en.wikipedia.org/wiki/Environmental_impact_of...

    The flushing flow method involves partially or completely emptying the reservoir behind a dam to erode the sediment stored on the bottom and transport it downstream. [7] [6] Flushing flows aim to restore natural water and sediment fluxes in the river downstream of the dam, however the flushing flow method is less costly compared to removing dams or constructing bypass tunnels.

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!